Endothelium-related Components of emphysema development in COPD and smoking [4, 10, 11, 12, 13, 18, 19, 20, 22, 23, 26, 27].
\r\n\t
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Venkateswarlu",coverURL:"https://cdn.intechopen.com/books/images_new/371.jpg",editedByType:"Edited by",editors:[{id:"58592",title:"Dr.",name:"Arun",surname:"Shanker",slug:"arun-shanker",fullName:"Arun Shanker"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"878",title:"Phytochemicals",subtitle:"A Global Perspective of Their Role in Nutrition and Health",isOpenForSubmission:!1,hash:"ec77671f63975ef2d16192897deb6835",slug:"phytochemicals-a-global-perspective-of-their-role-in-nutrition-and-health",bookSignature:"Venketeshwer Rao",coverURL:"https://cdn.intechopen.com/books/images_new/878.jpg",editedByType:"Edited by",editors:[{id:"82663",title:"Dr.",name:"Venketeshwer",surname:"Rao",slug:"venketeshwer-rao",fullName:"Venketeshwer Rao"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"4816",title:"Face Recognition",subtitle:null,isOpenForSubmission:!1,hash:"146063b5359146b7718ea86bad47c8eb",slug:"face_recognition",bookSignature:"Kresimir Delac and Mislav Grgic",coverURL:"https://cdn.intechopen.com/books/images_new/4816.jpg",editedByType:"Edited by",editors:[{id:"528",title:"Dr.",name:"Kresimir",surname:"Delac",slug:"kresimir-delac",fullName:"Kresimir Delac"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}}]},chapter:{item:{type:"chapter",id:"66804",title:"Smoking and COPD: Endothelium-Related and Neuro-mediated Emphysema Mechanisms",doi:"10.5772/intechopen.85927",slug:"smoking-and-copd-endothelium-related-and-neuro-mediated-emphysema-mechanisms",body:'\nEmphysema, or destruction of the gas-exchanging surfaces of the alveoli, is one of the typical manifestations of chronic obstructive pulmonary disease (COPD). Emphysema is a pathological term that is often used clinicaly, has great medical significance and describes only one of several structural abnormalities present in patients [1]. Many previous definitions of COPD have emphasized the terms “emphysema” and “chronic bronchitis,” which are not included in the definition used in the last GOLD report. In GOLD 2018, COPD was defined as a common, preventable, and treatable disease that is characterized by persistent respiratory symptoms and airflow limitation that is due to airway and/or alveolar abnormalities usually caused by significant exposure to noxious particles or gases [1]. It was mentioned that chronic respiratory symptoms also exist in individuals with normal spirometry and a significant number of smokers without airflow limitation have structural evidence of lung disease manifested by the varying presence of emphysema, airway wall thickening, and gas trapping [2, 3, 4]. Really, smoking is a major risk factor for COPD, and it plays an important role in lung tissue destruction development. Some experiments prove that aggressive pollutants of tobacco smoke (benzopyrene, peroxynitrite, acrolein, cyanides, peroxides, etc.) can cause direct damage to endothelial cells due to expression of adhesion molecules on their surface and intensification of lipid peroxidation [2, 5, 6, 7]. But the main underlying cause of structural changes is chronic inflammation, which is confirmed by numerous studies [1, 4, 5, 6]. Even in mild COPD, or in smokers susceptible to emphysema [7, 8], there are significant abnormalities in pulmonary microvascular blood flow that worsen with disease progression [9].
\nIt was proven that vascular endothelium actively participates in inflammatory reactions in COPD [10, 11, 12, 13]. It was a systemized data about cigarette smoke as an endothelial toxin and activator [14]. Endothelium is one of the direct participants of development and maintenance of chronic inflammation. Oxidized lipoproteins in the tunica intima of the vessel work as attractants for chemotaxis of leukocytes and monocytes that start to produce pro-inflammatory cytokines in big amounts. These processes trigger systemic inflammatory response that leads to irreversible thickening of the vessel walls and deterioration of their mechanical properties. Chronic exposure to tobacco smoke and the products of combustion of tobacco lead to chronic system inflammatory reaction, oxidative stress, endothelial dysfunction, and morphofunctional damage of target organs. Nowadays the connection between endothelium-related mechanisms and emphysema forming, and progression in COPD is well known. Recent studies are approaching the description of the neuro-mediated mechanisms of emphysema development in COPD.
\nIn this chapter we have analyzed data from researchers and shared our own research on the study of endothelium and the neuro-mediated mechanisms of emphysema development in COPD and smoking.
\nThe participation of endothelial dysfunction and injury in emphysema development in COPD has been described since 2000 and early [15, 16]. And the interest of researchers to the problem of the involvement of the endothelium in the pathogenesis of COPD has not decreased over the past decades. So, for the request “endothelium + emphysema” (in the title and/or abstract), the well-known online resource of the library PubMed offers 117 publications, of which 23 after 2015. For the request “endothelium + COPD,” it offers 335 publications, of which 72 after 2015, and for the request “endothelium + smoking,” it offers 1859 publications, of which 188 after 2015. This indicates the relevance of this area of research and demonstrates the hopes of researchers finding new opportunities for therapeutic and prophylactic effects on this relationship in the pathogenesis of tobacco-related lesions, COPD, and emphysema [17, 18, 19, 20, 21, 22, 23].
\nAll disorders begin with local and systemic inflammation, hypoxia and oxidative stress, and lead to an imbalance of proteases-antiproteases, loss of recovery and destruction of lung tissue. Activation and dysfunction of the endothelium involves, first of all, imbalance of the endothelium and its associated mechanisms, which are due to the following disorders in the pathogenesis of COPD [4]. Separately, we would like to pay attention on some endothelium-dependent factors.
\nProlonged damage to endotheliocytes by aggression factors (persistent inflammation, hypoxia, oxidative stress, an imbalance in the protease-antiprotease system, etc.) leads to their death and anatomical reduction of the capillary bed, which is a component of emphysematous lung changes. Pathobiology of small vessels in COPD, in addition to inflammatory and hypercoagulative changes, is characterized by intimal thickening, arteriole muscularization, a decrease in the number of capillaries, and a decrease in blood vessels [13, 15]. Delivering a VEGF receptor (VEGFR) antagonist to rats led rapidly to air space enlargement and pruning of the pulmonary arterial tree [23, 24]. VEGF is a trophic factor that is crucial for the survival of endothelial cells. The experiment demonstrated that prolonged blockade of VEGF receptors leads to apoptosis of septal endothelial cells and emphysema [16, 25]. Subsequent studies of emphysematous lungs confirmed that COPD patients have decreased lung levels of VEGF, reduced expression of VEGFR in pulmonary endothelial cells and apoptotic alveolar septal cells, and reduced expression of hypoxia-inducible factor-1α (HIF-1α), a transcription factor that drives the expression of genes involved in endothelial function including VEGFRs [26, 27]. It has been shown that along with the progression of emphysema, degenerative changes in the walls of the aorta develop, including its dilatation and aneurysmatization [28, 29]. These facts indicate that among other circumstances, an important role in the pathogenesis of emphysema belongs to endotheliocytes and VEGF. Moreover, it has been described that the presence of emphysema in patients with COPD is associated with a reduced content of сirculated endothelial cells, an endothelial repair factor [11, 30].
\nEndothelial dysfunction and damage are also caused by the acute effects of cigarette smoke long before the development of emphysema in animal models. Brief exposure of mice to cigarette smoke exacerbates lipopolysaccharide- and Pseudomonas aeruginosa-induced acute lung injury in vivo, and cigarette smoke extract increases the permeability of endothelial monolayers in vitro [14, 27]. Moreover, a recent study identified cigarette smoke-induced apoptosis of endothelial cells in the lungs of mice exposed chronically to cigarette smoke and COPD patients [11]. Thus, data from both animal models of COPD and COPD patients and controls support the hypothesis that endothelial dysfunction and injury are key processes in the pathogenesis of emphysema.
\nIn Table 1 we composed information on key endothelium-related agents that take into account the mechanisms of emphysema development in COPD, well described previously [4, 10, 11, 12, 13, 18, 19, 20, 22, 23, 26, 27].
\nComponents | \nOrigin, localization | \nPhysiological effects and potential role at pathogenesis emphysema in COPD | \n
---|---|---|
Nitric oxide (NO) | \nIn main, endothelial cells and other cells | \nVasorelaxation, vasoprotection, anti-inflammatory, anti-adhesion, reparation. Endothelin antagonist | \n
Endothelinum-1 (ET-1) | \nEndothelial cells, bronchial epithelium, alveolar macrophages | \nActivates receptors on smooth cells, encouraging stable vasoconstriction and increase of endothelium adhesively | \n
sPECAM-1 | \nEndothelial cells, lymphocytes, platelets, macrophages, granulocytes, T/NK-cell megakaryocytes, fibroblasts, osteoclasts | \nPlays a basic role in lymphocyte adhesion to vascular wall with followed effects | \n
Selectins: E-selectin (CD62Е), Р-selectin (CD62Р), L-selectin (CD62L) | \nActivated endothelial cells | \nRegulation of leukocyte adhesion (strengthens the capacity to migration, leukocyte adhesion to activated endothelium in inflammation) | \n
Thrombomodulin (CD141) | \nEndothelial cells | \nInteracts with thrombin, activates protein C, acts as anticoagulant across activation factors fVa, fVIIIа, fXa, and fXIIIa | \n
Circulated endothelial cells | \nEndothelial cells from vascular wall, activated bone marrow | \nCan be as the factor of reparation according to inflammatory processes and as the factor of injury to the endothelium and other tissues due to activated phenotype | \n
Vascular endothelial growth factor (VEGF) | \nEndothelial cells | \nMain inductor of angiogenesis, VEGF, provides their effects across receptors’ endothelial cell and expression of VEGF regulated by hypoxia, chronic inflammation, hypercoagulation, etc. In chronic processes, function can be an imperfect character Stimulates apoptosis and phagocytosis and promotes development of emphysema | \n
Neutrophil elastase (catepsin G, proteinase 3) | \nNeutrophils, monocytes, Т lymphocytes, endothelial cells, vascular smooth muscles cells | \nDecreases migration of T lymphocytes and neutrophil to inflammation area, factor of decelerating of phagocytosis. Function from protection to damaging. Can cause damage to tissues, development of emphysema, and mucus hypersecretion Involved in normal degradation of matrix proteins elastin, collagen, fibronectin, laminin, and proteoglycans | \n
Matrix metalloproteinases (ММP-1, ММP-2, ММP-9) | \nEndothelial cells, macrophages, neutrophils, monocytes, fibroblasts, keratinocytes, osteoblasts | \nContributes to release TNF-α from macrophages, that results to neutrophils recruiting and production neutrophil elastase, that leads to damage tissues, development emphysema. Involved in degradation of type IV collagen, fibronectin, and elastin | \n
The mechanisms of the inclusion of neurokinins and related substances in neurogenic inflammation and destruction at different stages of COPD are much less known. Moreover, in recent studies, descriptions of the neuro-mediated mechanisms for the development of emphysema in COPD and smoking have become recognized.
\nIt is known that tobacco smoke is a powerful inducer of the destruction of the respiratory epithelium throughout, followed by its morphofunctional remodeling [4, 31, 32]. Initiation of cell and tissue injury processes in prolonged exposure to smoking can take place due to excess release of neurotransmitters from sensitive afferent nerve fibers of the nervous vagus system. A large proportion (75%) of such fibers belong to the type of nonmyelinated or C-fibers, the sources of which are small neurons of the knotted and jugular ganglia, which synthesize neuropeptide transmitters or neurokinins (such as substance P (SP), a peptide genetically related to calcitonin (CGRP) and neurokinin (A)) [33, 34]. Afferent influences are primarily aimed at maintaining the structural and functional homeostasis of the respiratory system by stimulating the secretion of mucus from the submucous glands and goblet cells, contractility of smooth muscles, vascular permeability, modulation of immune cascades, etc. [34, 35, 36]. It is known that afferent fibers (C-fibers) are extremely sensitive to the effects of irritants that make up tobacco smoke [37]. In a situation of prolonged and/or intense stimulation of sensory fibers, excessive release of neuropeptide mediator is accompanied by a number of plastic and destructive processes due to a cascade of pathological reactions of neurogenic inflammation [38, 39]. In addition to substance P of neuronal origin, neuropeptides from cells of the immune system—eosinophils, basophils, monocytes, macrophages and lymphocytes—join the realization of neurogenic inflammation [38, 40, 41]. The obtained data indicate the role of the disturbance of the activity of the neurokinin system in the development and maintenance of morphofunctional changes in the pathology of the respiratory tract associated with smoking [42, 43, 44, 45, 46]. Chronic exposure to cigarette smoke has been shown to increase SP expression in neurons of the central nervous system [35, 36, 37] and simultaneously inhibits the activity of enzymes that metabolize neurokinins [39, 40, 43]. According to experimental study, even low concentrations of cigarette smoke significantly reduce the topical activity of neuronal endopeptidase and increase the concentration of CP in the respiratory tract [35]. The contribution of excessive sensitivity of NK1 receptors in the airways to the development of bronchoconstriction under the influence of tobacco smoke irritants and/or during bronchial asthma has been proven [42, 43, 47]. At the same time, the components and mechanisms of neurogenic inflammation in the development of emphysema associated with prolonged exposure to tobacco smoke are poor and fragmentary in the literature.
\nIn Table 2 we have tried to compose information about potential neuro-mediated mechanisms of emphysema development in COPD and tobacco smoking.
\nAgents | \nOrigin, localization | \nPhysiological effects and potential role in emphysema pathogenesis in COPD | \nReferences | \n
---|---|---|---|
Neurokinins Substance P (SP) | \nSensitive nerve endings. SP receptors on respiratory and glandular epithelial cells and endothelial cells. Neurokinin receptor-1 affixed to SP is found in submucous glands, and SP release from nociceptive nerves is responsible for secretion of glands | \nBelongs to the family of tachykinins, sensory peptides. Induces vasodilation and transudation of blood plasma in the respiratory tract. Induces chemotaxis of monocytes, neutrophils, and eosinophils and stimulates macrophages to produce mediators of inflammation and neutrophil elastase. Powerful mast cell stimulator, causing their degranulation. Sources and release of histamine and cytokine synthesis (IL-6). Takes part in neurogenic inflammation when stimulating the production of IgA from B lymphocytes and cytokines from T-helper cells. Enhances the release of acetylcholine from the postganglionic cholinergic nerves of the respiratory tract It causes smooth muscle contraction, secretion of submucous glands, vasodilation, and increased vascular permeability. Tobacco smoking inhibits the activity of the enzyme endopeptidase, which enhances the activity of SP | \n[40, 45, 48, 49] | \n
Neurokinins Neurokinin А | \nThe highest density in the nerve fibers around the arteries. Tachykinin receptor subtypes NK1, NK2, and NK3 | \nBelongs to the family of tachykinins, sensory peptides. Contraction of smooth muscles; secretion of submucous glands; vasodilation; increased vascular permeability; stimulation of cholinergic nerves, mast cells, B and T lymphocytes, and macrophages; eosinophil chemoattraction; and adhesion of neutrophils in the vessels of the respiratory tract with activation following | \n[44, 50, 51] | \n
Neuropeptide -γ | \nIt is produced in some of the upper cervical ganglia and the bodies of the main palatine cells Sympathetic nerves contain either norepinephrine or norepinephrine and neuropeptide Y | \nReduces the frequency of vibrations of ciliary cells induced by cholinergic nerves, providing an inhibitory effect on these nerves Sympathetic reflexes cause vasoconstriction and can also stimulate the secretion of certain glands in the trachea and bronchi | \n[38, 39, 48] | \n
Receptor NK1 | \nNK1 tachykinin receptor mRNA is found in the pulmonary arteries, veins, and human bronchi, in the endothelium of the veins and arteries, and in the smooth muscles of the bronchi, as well as in lymphocytes, macrophages, and mastocytes | \nThe tachykinin receptor NK1, with the highest affinity for SP. SP, in turn, is a powerful mast cell stimulator, causing their degranulation, and induces the chemotaxis of monocytes, neutrophils, eosinophils, and stimulates macrophages to produce inflammatory mediators and neutrophilic elastase | \n[40, 42, 45] | \n
Receptor NK2 Receptor NK3 | \nNK2 receptor mRNA is abundantly expressed in the human bronchi and weakly in the pulmonary veins and arteries NK3 tachykinin receptor mRNA is found in the pulmonary arteries, veins, and human bronchi | \nThe tachykinin receptor NK2, with the highest affinity for neurokinin A. Tachykinin receptor NK3, with the highest affinity for neurokinin B The release of histamine from mouse mast cells is mediated through tachykinin NK2 receptors | \n[40, 42, 45, 52] | \n
Potential neuro-mediated mechanisms of emphysema development in COPD and tobacco smoking.
To study the contribution of the components of neurogenic inflammation to the processes of tissue remodeling in pulmonary emphysema associated with smoking, an experimental model of long-term tobacco smoking in vivo in rats was reproduced. The experiment was performed in appliance with the model D. According to Zheng [53] in our own modification [54], the duration of exposure to tobacco smoke in terms of human life is 12 years. The features of the distribution and activity of SP, NK1, MMP-2, MMP-9, and TIMP-2 in the tissues of the mucous membrane of the lungs were performed using the immunoperoxidase method on cryostat sections of 15 μm in thickness according to standard methods. The following primary antibodies were used: anti-SP (Abcam, ab 14184, 1:200, США), anti-NK1 (Chemicon AB 5060, 1:500, USA), anti-MMP2 (rabbit polyclonal, ThermoScientific), anti-MMP9 (rabbit polyclonal, ThermoScientific, rb-9234-p, 1:200), anti-TIMP2 (rabbit polyclonal, Abcam, ab61224, 1:100), secondary biotinylated antibodies (ThermoScientific, 1:200), streptavidin peroxidase (ThermoScientific), and chromogen (Peroxidase Substrate Kit, VectorNovaRED, SK-4800). Morphological studies were performed in the laboratory of the Pacific State Medical University.
\nThe results of morphological studies of the bronchopulmonary system of rats in the control group and with the model of long-term tobacco smoking are presented in Figure 1.
\nThe lung (A, B) and bronchi (C, D) of animals in the control group (A, C) and rats with the DTC model (B, D). Coloring: hematoxylin-eosin. Scale: A, B (500 microns); C, D (100 microns).
Morphological changes in the lungs of rats with a long-term tobacco smoking model are focal. Over the entire area of the slice of the lungs, there are fields with pronounced emphysematous changes, accompanied by loss of the integrity of the alveoli and the formation of large emphysematous expansions, an increase in the thickness of the interalveolar septa (Figure 1B,D). In other parts of the lung parenchyma, there are signs of swelling and/or hemorrhagic impregnation in peribronchial spaces. Cellular composition contains cells of immune inflammation—plasma cells, lymphocytes, and macrophages.
\nThe distribution of the components of the neurokinin system of rats obtained by morphological examination of the bronchi and lungs coincides with the previously described data [55] and is shown in Figure 2. Nerve fibers secreting SP are presented in the subepithelial zones of the bronchi (Figure 2A); their penetration is recorded in the epithelial layer (Figure 2B), pulmonary parenchyma (Figure 2D), and adventitia of pulmonary vessels (Figure 2E).
\nDistribution of SP- and NK1-reactive structures in the bronchopulmonary system of rats. Coloring: immunoperoxidase reaction on SP; repainting, hematoxylin-eosin. Scale: A, 100 microns; B–E, 50 microns.
The morphometry of the components of the neurokinin system in the bronchopulmonary system of rats was compared with the model of long-term tobacco smoking and control animals (Table 3).
\nIndicator | \nBronchi | \nLungs | \n||
---|---|---|---|---|
Control | \nExperiment (long-term smoking model) | \nControl | \nExperiment (long-term smoking model) | \n|
SP distribution area (%) | \n5.11 ± 0.36 | \n5.59 ± 0.14*\n | \n4.60 ± 0.29 | \n5.10 ± 0.34*\n | \n
NK1 distribution area (%) | \n0.27 ± 0.03 | \n0.31 ± 0.03*\n | \n0.16 ± 0.016 | \n0.16 ± 0.02 | \n
NK1-positive mast cells (in 1 mm3 of the tissue) | \n\n | \n | 92.68 ± 19.26 | \n76.39 ± 15.74*\n | \n
General population of tissue basophils (in 1 mm3 of the tissue) | \n\n | \n | 129.53 ± 19.64 | \n106.93 ± 7.64*\n | \n
Morphometric characteristics of SP- and NK1-immunoreactive structures in the bronchopulmonary system of rats.
The differences are significant with р < 0.05.
The content of SP-containing fibers and NK1-positive structures in the control group and in the model of long-term tobacco smoking shows an ambiguous pattern. An increase in the distribution area of SP-immunopositive nerve fibers in the lungs and bronchi of experimental animals was found to be 10.7 and 9.4%, respectively, compared with the control group. The most significant increase in fiber density was observed in the adventitia of pulmonary parenchyma vessels compared with other structures. Being a vasodilator, substance P increases vascular permeability and promotes adhesion and penetration of leukocytes into the surrounding tissues for the realization of local immune reactions involved in the development of destructive processes in the pulmonary parenchyma. Regarding NK1-positive elements, it should be noted that there is no change in their content in the lung tissue and a moderate increase in the density in the bronchial wall against the background of a decrease in the total number and NK1-immunoreactive tissue basophils. Obviously, substance P plays a key role in the implementation of neurogenic inflammation processes in chronic exposure to tobacco smoke. The established pattern of changes in NK1-positive structures can be explained by the ability of SP to cause mast cell degranulation and NK1 receptor-dependent release of histamine and serotonin involved in local inflammatory answer.
\nOne of the leading stimulators of the synthesis of substance P in the model of long-term tobacco smoking is hypoxia which changes the humoral regulation of blood flow [55]. SP can adjust the change in vessel diameter at the unchanged vascular wall using an axon reflex for adequate blood flow at a given point in time. However, when the architectonics of the vascular wall changes, the SP loses its function as a regulator and can participate in both excessive vasodilation and paradoxical vasoconstriction.
\nIn the development of the structural remodeling of the respiratory system, there are several morphological phenomena that accompany this process and are the basis for the development of reversible and irreversible morphofunctional changes. These include thinning of the epithelial layer, development of subepithelial fibrosis, an increase in smooth muscle thickness, an increase in the number and/or size of the submucosal glands, and the activation of angiogenesis processes [56]. In the pathogenesis of the changes taking place, great importance is attached to the activity of the enzymes of the extracellular matrix, which ensure the degradation of its interstitial proteins. Modern advances in proteomics have shown that for normal development, physiological renewal, restoration of healthy tissues, and the formation of pathological changes in tissue morphology, two groups of proteins are leading—MMPs and their tissue inhibitors [57, 58]. MMPs are a family of 20 zinc and calcium-dependent endopeptidases capable of cleaving almost all components of the extracellular matrix of connective tissues [59]. The level of synthesis and secretion of MMP into the extracellular space is regulated by transcription factors, and their proteolytic activity depends on the chemical transformations of the enzyme molecule in the interstitial space. As a result, either activation of the proenzymes or inhibition of their active forms can be observed. Depending on the type of protein metabolized, MMP can be divided into collagenases (MMP-1, MMP-8, and MMP-13), gelatinase (MMP-2 and MMP-9), stromalins (MMP-3 and MMP-10), etc. [60, 61]. In mammals there are four known TIMPs that inhibit all MMPs in a 1:1 ratio by strong covalent bonding [62]. It is believed that the balance of proteolytic and antiproteolytic mechanisms maintained in different tissues and organs is carried out by a specific set of intercellular matrix enzymes and their inhibitors [59, 63]. On the other hand, each process has a specific set of depressed matrix proteolytic enzymes. In this regard, great prospects in creating targeted therapy for many pathological processes are associated with the determination of the tissue specificity of the enzymes of the extracellular matrix and the identification of patterns of changes in their activity during the development of pathology.
\nA number of studies have shown the role of individual types of MMP in the development of nicotine-associated pathology of the lungs and bronchi [57, 58]. To clarify the role of the leading MMP—MMP9 related to the inducible form and MMP2—considered as a constitutive variant of the enzyme in the development of pulmonary emphysema associated with long-term smoking, we studied the immunohistochemical and biochemical content of enzymes in the tissues and homogenates of rats with long-term smoking patterns (Figure 3).
\nImmunohistochemical (A–C) and biochemical determination of MMP in the bronchopulmonary system of rats with a model of long-term tobacco smoking. Coloring—immunohistochemical reaction to MMP-2 and MMP-9. Scale: A, B, B—50 μm. Localization of MMP-2 in the wall of the bronchus (A, B) and interalveolar septa (C). (D) Zymogram of MMP-2 and MMP-9. Lanes 1–4, lung homogenates of rats of the control group; lanes 5–8, lung homogenates of rats with a model of long-term tobacco smoking.
In the bronchopulmonary system of rats, prolonged exposure to tobacco smoke is accompanied by ambiguous dynamics of the content of matrix metalloproteinases and their inhibitors. Normally, the activity of MMP-2 and MMP-9 is recorded in the cytoplasm and processes of bronchial and pulmonary fibroblasts, which form a thin MMP-positive strip in the lamina propria of the bronchial mucosa (Figure 3A,B) and in the interalveolar septa (Figure 3C). In the lungs and bronchi of rats with the long-term tobacco smoking model, a marked decrease in the immunohistochemical activity of MMP-2 and MMP-9 was observed. At the same time, in the acute phase of the experiment, the number and intensity of coloring of immunopositive structures on MMP-2 and MMP-9 are higher than in the control group. According to the quantitative determination of enzymes in the homogenates of lung tissue (Figure 3D, Table 4), the resulting trend is confirmed. That is, with the development of pulmonary emphysema associated with prolonged smoking in the lung tissue, the content of both MMPs decreases evenly.
\nIndicators | \nControl | \nExperiment (long-term smoking model) | \nControl | \nExperiment (long-term smoking model) | \n
---|---|---|---|---|
ММР-9 | \nММР-2 | \n|||
Conventional density units | \n742689.75 | \n450081.25*\n | \n367243.25 | \n246414.75*\n | \n
ММР-9/ММР-2 | \n2.02 (control) | \n1.83 (experiment (long-term smoking model)) | \n
The contents of MMP-2 and MMP-9 in the homogenates of the lungs of rats.
The differences are significant with р < 0.05.
An analysis of the immunohistochemical composition of the tissue inhibitor of both MMP and TIMP-2 showed a marked decrease in its representation in the structures of the bronchopulmonary system of animals on a model of long-term smoking (Figure 4).
\nThe distribution of the content of TIMP-2 in the lungs of rats of the control (A–C) and with the model of long-term tobacco smoking (D) groups. Coloring—immunohistochemical reaction to TIMP-2. Scale A, 100 microns; GD, 50 microns. A total enzyme content in the tissues of the bronchopulmonary system. B-TIMP-2-positive fibroblasts of the interalveolar septa. B-content of the enzyme in the epithelial cells of the small bronchus (indicated by arrows). G-reduction of the enzyme content in epithelial cells of the bronchus of rats with a model of prolonged smoking (indicated by arrows).
In intact animals, the enzyme localization occurs in the respiratory epithelial cells of the bronchial membrane (Figure 4C, indicated by arrows) and fibroblasts of the interalveolar septa (Figure 4B). In animals of the main group, the overall intensity of immunohistochemical staining of lung tissue decreases, and at high magnifications of the microscope, it is possible to fix a significant depression of the color or complete disappearance of the enzyme content in the epithelial lining cells of the bronchi and lung parenchyma tissue (Figure 4, indicated by arrows).
\nAccording to the data obtained, the immunolocalization of MMP-2, MMP-9, and TIMP-2 repeats the basic pattern of distribution of pro-inflammatory cells and coincides with the foci of the most noticeable rearrangements of the connective tissue of the bronchi and the pulmonary parenchyma. In the acute phase of the experiment, the activity of the markers is significantly higher compared to the control; after 6 months of exposure to smoke, there is a decrease of the proteolytic activity and at the same time the processes of its inhibition.
\nIn addition to studying the processes of neurogenic inflammation and the contribution of matrix metalloproteinases to the development of emphysema in the experiment, we analyzed the content of neurokinin system markers, the localization, and the content of MMP-2, MMP-9, and TIMP-2 in human lung tissue structures. Morphological studies of autopsy material were performed on 12 individuals aged 51–65 years and 3 women and 9 men, average age 61.5 ± 4.14 years, who died a sudden death outside the hospital. The long-term history of tobacco smoking was clarified from the close relatives and on the basis of the data of the outpatient card. Features of the distribution and activity of SP, NK1, MMP-9, and TIMP-2, in lung tissues were investigated using the immunoperoxidase method on cryostat sections of 15 μm in thickness according to the standard procedure using the primary antibody line described above.
\nIn lung tissue and bronchial wall of patients with pulmonary emphysema, positive SP immunoreactivity is found mainly in the nerve fibers (Figure 5). More common are single conductors having a uniform ribbonlike course and numerous varicose thickenings. With a successful coincidence of the cut plane with the spatial geometry of the fibers, it is possible to observe beams extending 300–500 μm. Fibers penetrate through the walls of the bronchi of medium and small caliber, spread around the perimeter of the submucosa (Figure 5A, B). In the interstitial tissue, lightweight fibers have a diameter of 0.5–1 microns, and sometimes they are grouped into clusters with the formation of numerous terminals. Probably, the latter are areas of the most dense accumulation of neuromuscular and glandular contacts. The morphological characteristics of the colored conductors allow them to be treated as mixed (afferent and motor) fibers. High SP expression is also detected in peribronchial leukocyte infiltrates (Figure 5D). Here, high immunoreactivity is observed for neurokinin receptors of type 1 (Figure 5B,D). The preferential localization of the NK1 surface of the membranes of the secretory epithelial cells of the bronchial glands, alveolar and stromal macrophages, microvascular endothelial cells, and elements of the fibrocartilage membrane (Figure 5B,D,E,H) should be emphasized.
\nDistribution of the content of SP (A, C, E, G) and NK1 (B, D, F, H) in the bronchopulmonary system in persons with emphysema. Coloring: immunohistochemical reaction to SP and NK1, stained with hematoxylin. Scale: A, B, E, G (50 microns); C, D (100 microns); and F, H (20 microns). Nerve fibers innervating the wall of the bronchus (A) and interalveolar partitions (C). Localization of SP-positive macrophages in peribronchial infiltrates (E). SP-positive glandulocytes of the bronchial glands (G). Localization of neurokinin receptors on the surface of peribronchial macrophages (B), dust macrophages (D), vascular endothelial cells (F), and chondrocytes of the fibrocartilage membrane of the bronchi (H).
Prolonged pathological effects of tobacco combustion products entail the formation of structural changes with the active involvement of the neurokinin innervation apparatus localized in the mucous membranes of the respiratory system. The increase in the number of macrophage cells and NK1-positive macrophages, and the direct interaction between them and afferent fibers, through terminals, suggests the involvement of sensory nerve fibers in the regulation of local immune, inflammatory, and destructive processes in the lung tissue during smoking-induced emphysema.
\nIn contrast to the experimental data, in individuals with long periods of smoking and emphysema, there is an increase in the immunohistochemical density of MMP-9 in the pulmonary parenchyma (Figure 6), while TIMP-2 is practically undetermined (Figure 7).
\nLocalization of MMP-9 in the lungs (A, B) of a person. Coloring: immunohistochemical reaction to MMP-9, stained with hematoxylin. Scale: A (50 microns); B (100 microns).
Localization of TIMP-2 pulmonary parenchyma in individuals with emphysema. Coloring: immunohistochemical reaction to TIMP-2, stained with hematoxylin. Scale: 100 microns.
In this way, from the presented data of experimental modeling of emphysema associated with long-term smoking, as well as studies in people with pulmonary emphysema and long-term tobacco smoking experience, neurogenic inflammation takes an active part in the processes of remodeling of lung tissue. Markers of neuro-mediated inflammation activity are overexpression of SP-containing nerve fibers, the presence of NK-1-tagged macrophages, mast cell degranulation, and an immune-mediated pattern of inflammatory infiltrate. Pathomorphosis of pulmonary parenchyma destruction in nicotine-associated pulmonary emphysema is associated with dysregulation in the state of the family of matrix metalloproteinases. In the acute period of exposure to tobacco combustion products, overexpression of MMP-9 is observed with suppression of the activity of the tissue inhibitor TIMP-2, followed by depression of the tissue content of both MMP-2 and MMP-9 and an inhibitor of their activity TIMP-2. In individuals with pulmonary emphysema, the MMP-9 tissue pattern retains its excessive representation.
\nResults from human and animal studies indicate that endothelial dysfunction and injury contribute not only to the genesis and progression of pulmonary lesions in COPD (especially emphysema development) but may also contribute to some of the common comorbidities and systemic effects reported in COPD patients. Vascular endothelium initiates and modulates the main pathomorphic processes in COPD and smoking. In particular, endothelium activation is an important factor of initiation, development and persistence of inflammation, and vessel and tissue remodeling, in particular emphysema. It is not by chance that the relationship of emphysema of the lungs is described in violation of the mechanical properties of the aorta and excessive stiffness of other exponents’ bloodstream [4, 6, 64]. At the basis of these pathological processes are common (genetically determined and pathologically determined) mechanisms associated with impaired collagen-elastin metabolism.
\nThe latest studies are conducted in the direction of studying not simple, associated with the endothelium, but specific neuro-mediated mechanisms of emphysema development in COPD and smoking. Our studies presented in this chapter describe the study of the processes of neurogenic inflammation and the contribution of matrix metalloproteinases to the development of emphysema in the experiment and in humans.
\nWe are confident that there is a special morphofunctional continuum in the development of lower respiratory tract remodeling in response to chronic exposure to tobacco smoke and the development of inflammation in COPD. New data suggest that imbalance of neuro-mediated interactions, alteration of vasomotoric signaling mechanisms, secretion, mucociliary clearance, cytoprotection involving substance P-dependent components with impaired content, and development of dystopia of matrix metalloproteinases and their tissue inhibitors are involved in the initiation of morphological restructuring. Future studies should also assess the extent to which endothelial dysfunction and injury, particularly neuro-mediated mechanisms, underlie emphysema in COPD and smoking as target to therapeutic and prophylactic impacts.
\nNo any conflict of interests.
COPD | Chronic obstructive pulmonary disease |
VEGF | Vascular endothelial growth factor |
VEGFR | VEGF receptor |
NO | Nitric oxide |
ET-1 | Endothelinum-1 |
sPECAM-1 | Soluble platelet endothelial cell adhesion molecule |
VEGF | Vascular endothelial growth factor |
ММP | Matrix metalloproteinases |
SP | Substance P |
Upwelling is an important oceanographic phenomenon that refers to an upward movement of seawater, with a typical speed of order 10−6~10−4 m/s. Accompanied by the upwelling process, the subsurface/deep cooler, and normally nutrient-rich, water rises toward the ocean surface, leading to a background with high biological productivity that is beneficial for the growth of phytoplankton and other primary producers. Therefore, good fishing grounds are commonly found in the vicinity of upwelling regions. From the dynamical point of view, major mechanisms for the generation of the coastal upwelling include the alongshore wind and wind stress curl, although other factors (e.g., tides, topography, and river discharge) also play considerable roles depending on the regions under investigation [1].
The coastal upwelling of cold and nutrient-rich waters off the China coasts is significant not only for the regional fishing industry, but also for the global carbon cycle and thus for the Earth’s climate. Therefore, the coastal upwelling becomes a research hotspot of coastal oceanography in China, which has attracted great attention for recent decades. For example, Miao and Hu [2] analyzed the characteristics of wind-driven coastal upwelling off the southeastern China coast using coastal upwelling index (CUI) data, which are calculated online the Pacific Fisheries Environmental Laboratory (PFEL) website (
Monthly mean coastal upwelling index (b) off the southeastern China coast (the station locations for calculating the coastal upwelling index are shown in panel (a)). Redrawn from Miao and Hu [2].
Hu and Wang [1] reviewed the progress of upwelling studies in the China seas since 2000 and summarized 12 major upwelling regions in the China seas, including the South China Sea (SCS), the Taiwan Strait (TWS), the East China Sea (ECS), the Yellow Sea, and the Bohai Sea (Figure 2). Half of these upwelling regions are located along the southeastern coast of mainland China, that is, the upwelling off the Yangtze River Estuary, the upwelling along Zhejiang coast, the upwelling regions along the northwestern and southwestern coasts of Taiwan Strait, the upwelling along the eastern Guangdong coast, and the upwelling around the eastern Hainan Island. It is concluded that these coastal upwellings are principally wind-driven, and are hence strongly related to the seasonal variability of monsoon winds.
Map of major upwelling regions in the China seas, including the South China Sea (SCS), the Taiwan Strait (TWS), the East China Sea (ECS), the Yellow Sea (YS), and the Bohai Sea (BS). In this figure, the Yangtze River Estuary and the Pearl River Estuary are indicated by YRE and PRE, respectively. PM stands for the Peninsular Malaysia; LZS for Luzon Strait; and LS, NR, and SA for Lüsi, Nanri, and Sabah, respectively. The red ellipses or circles schematically mark locations of the major upwelling regions in the China seas. The ellipses or circles in dashed lines are upwelling regions that are sometimes mentioned. Cited from Hu and Wang [1].
In this chapter, we describe six major coastal upwelling regions off the southeastern coast of mainland China and discuss the influence factors for these coastal upwelling regions.
Published about 15 years ago, Wu and Li [4] and Li et al. [5] overviewed studies of upwelling in the SCS over four decades among 1964–2003, focusing primarily on the spatiotemporal variability of upwelling in the continental shelf of the northern SCS. They pointed out that in summer upwelling occurs over almost the entire continental shelf of the northern SCS. Figure 3 presents the locations of some upwelling regions, investigated by several representative studies [6, 7, 8, 9, 10]. Most of these upwellings have been demonstrated to be induced by the prevailing southwesterly monsoon. Since then, much progress on the coastal upwelling study has been intensively made in the northern SCS using cruise observations, satellite observations, and numerical modelling.
Reported upwelling regions in the continental shelf of the northern SCS. Redrawn from Wu and Li [4]. It summarizes the research included in [6, 7, 8, 9, 10]. PRE stands for the Pearl River Estuary; LZ for the Leizhou Peninsula; DS, ST, HL, SW, and DY for Dongshan, Shantou, Huilai, Shanwei, and the Daya Bay, respectively.
Over the past two decades, a number of hydrography-oriented cruises have been conducted in the continental shelf of the northern SCS. These data further evidenced the upwelling and its variability. Using underway measurements of sea surface temperature and salinity collected during July–August 2000, Zhuang et al. [11] observed an evident upwelling-related, low-temperature, and high-salinity area along the coast between Dongshan and Huilai (see locations in Figure 2 or 3). Based on the hydrological data from a cruise during July–August 2002, Xu et al. [12] analyzed the upwelled cold water along the eastern coast of Guangdong, and found that cold cores were distributed near the Daya Bay and the Huilai coast. Upwellings off the Pearl River (also called the Zhujiang River) Estuary were examined during different monsoon periods in July 2000 by Zeng et al. [13], and in May 2001 and November 2002 by Zhu et al. [14], respectively. Zhang et al. [15] investigated hydrological (including upwelling) characteristics off the Pearl River Estuary using data from two cruises in summer and winter 2006. Cai et al. [16] and Wan et al. [17] analyzed the characteristics of upwelling in the eastern Guangdong and southern Fujian coastal waters using the comprehensive cruise data; their results illustrated the coastal upwelling between Shantou and Dongshan undergoing an alternating strong-weak-strong stage during July–August 2006. Based on the conductivity-temperature-depth (CTD) data from the summer cruises of 2001, 2002, 2006, and 2009, Xu et al. [18] revealed the interannual variation in the spatial structure and intensity of upwelling in the eastern Guangdong and southern Fujian coastal seas. The abovementioned cruise data confirmed that the summertime coastal upwelling is conspicuous along the coasts of eastern Guangdong and southern Fujian, with the former occurring earlier and stronger than the latter.
Using satellite remote sensing data, combined with shipboard measurements conducted in July 2000, Zhuang et al. [19] analyzed upwelling phenomena off the Fujian and Guangdong coasts. Qiao and Lü [20] applied satellite sea surface temperature (SST) and chlorophyll-a (Chl-a) data from different sources to summarize some basic characteristics of the coastal upwelling in the SCS. Applying the Quick Scatterometer (QuikSCAT) wind data, Wang et al. [21] examined relative roles of Ekman transport and Ekman pumping in driving summer upwelling. These results indicated that the coastal upwelling often occurs in the coastal area around the eastern Hainan Island and in the waters along eastern Guangdong and southern Fujian coasts in summer, which may be resulted from multiple dynamic factors such as wind forcing, tidal mixing, and the interactions between local circulation and topography. However, the coastal upwelling in the eastern Guangdong is primarily driven by Ekman transport.
Several numerical models have been applied to study the upwelling and its mechanism in the northern SCS since 2000. For example, Chai et al. [22] simulated several upwelling regions in the SCS using the Princeton Ocean Model (POM), and explained their mechanisms. Jing et al. [23, 24] studied the summer upwelling system in the northern continental shelf of the SCS using a three-dimensional (3D) baroclinic nonlinear model. Zhang and Jiang [25] studied the mechanism of cross-shelf transport of the cold bottom water (upwelling water) on the coastal shelf off Shanwei using the Regional Ocean Modeling System (ROMS). These model results showed that the summertime upwelling is a common phenomenon during June–September east of the Hainan Island and the Leizhou Peninsula, and in the coastal areas from Shantou to Nanri. Both southwesterly wind and wind stress curl are responsible for generating the coastal upwelling east of Hainan, while the wind-driven cross-shelf Ekman transport is a significant dynamic factor to the coastal upwelling off the eastern Guangdong and southern Fujian coasts.
The upwelling off the eastern coast of Hainan Island is strong in summer, which has attracted a lot of intensive studies for recent years [26]. Specifically, Chai et al. [27] simulated the upwelling using the POM; Su and Pohlmann [28] applied a 3D high-resolution model to study the upwelling mechanism; Li et al. [29] investigated the spatial structure and variation of the summertime upwelling in the waters east and northeast of Hainan Island during 2000–2007 by using a nested high-resolution POM forced by QuikSCAT winds; Wang et al. [21] estimated the mean Ekman transport and Ekman pumping in the coastal waters east and southeast of the Hainan Island; Lin et al. [30, 31] compared the upwelling patterns in the eastern and northeastern Hainan Island using a combination of cruise observations, reanalysis data and satellite data, and studied the mechanism for the upwelling off the northeastern coast of Hainan Island with a numerical model. These results suggested that the coastal upwelling off the eastern coast of Hainan Island usually exists from April to September, with the strongest intensity in summer; the upwelling is mainly induced by summer monsoon wind. By contrast, Jing et al. [24] proposed that the Ekman pumping associated with the local wind stress curl is a key factor modulating the generation of the coastal upwelling off eastern Hainan Island and eastern Leizhou Peninsula. Based on the cruise data in summer 2006, together with the QuikSCAT winds, Xu et al. [32] pointed out that the coastal upwelling regions are merged below 10 m layer in the waters off eastern Hainan and western Guangdong, and that the coastal upwelling off eastern Hainan Island is intermittent and modulated by the alongshore wind while that off the western Guangdong is mainly induced by the wind stress curl.
On upwelling variability, Liu et al. [33] studied the variability of summer coastal upwelling in the northern SCS during the last 100 years. Jing et al. [34] identified that the coastal upwelling in the northern SCS was closely linked to the modulation of El Niño events; they found that during the summer of 1998 (a La Niño year), the coastal upwelling was greatly strengthened associated with an abnormally intensive alongshore wind stress blowing over the region. Su et al. [35] studied the variation of coastal upwelling off the eastern Hainan coast over 50 years of 1960–2006 using an “SST upwelling index”. By using an SST record (AD 1876–1996) derived from coral Porites Sr/Ca, Liu et al. [36] revealed that upwelling in the northern SCS underwent a distinct multidecadal variability, which was proved to be caused by the Asian summer monsoon with an abrupt shift in 1930 from a relatively warm to cold condition, and then back to the warm condition after 1960. These results showed a general intensifying of coastal upwelling off eastern Hainan Island subject to prominent interannual and decadal variations; the intensifying trend was also consistent with the global warming in the twentieth century.
Xiao et al. [37] and Hu et al. [38] collected many papers and comprehensively reviewed the upwelling studies in the TWS mostly before 2000, and also proposed suggestions for upcoming investigators. The reviews showed that the main coastal upwelling regions (Figure 4) in the western TWS are located near Dongshan and Pingtan. Over the past two decades, some progress has been made in studying the TWS upwelling, especially on its variability, mechanism and responses to the El Niño-Southern Oscillation (ENSO), and local environmental variation.
Schematic map of main upwelling regions in the TWS. Redrawn from Hu et al. [38]. DS: Dongshan; MZ: the Meizhou Island; NA: Nan-ao; PH: the Penghu Islands; PT: Pingtan; TB: the Taiwan Bank; XM: Xiamen. Four ellipses and circle schematically indicate the locations of four upwelling regions.
Strong coastal upwelling usually appears in the western TWS during the summer southwesterly monsoon period, which has been confirmed by a number of hydrological and satellite observations in the last decades (e.g., [39, 40, 41, 42, 43, 44, 45]). These studies showed that the intensity of coastal upwelling is affected by many factors, such as the northward or northeastward current, southwesterly monsoon, and bottom topography. Recently, more attention has been paid to the variability of the coastal upwelling in the western TWS. Three examples are given next.
Hong et al. [46] studied the interannual variability of summer coastal upwelling in the TWS using a long time series of SST data from 1985 to 2005. It is shown that in some years, the coastal waters near Pingtan or Dongshan had clear upwelling signatures at the sea surface with a negative temperature anomaly and positive salinity anomaly. The alongshore wind stress was demonstrated to be responsible for such interannual variations.
Hu et al. [47] studied the variable hydrographical structure in the southwestern TWS using measurements from four summer cruises in 2004–2007, and revealed that the coastal upwelling near Dongshan occurred with different scales, locations, and intensities. Evident coastal upwelling was seen in the southwestern TWS during each July of 2005 and 2007, and was largely associated with local wind condition as confirmed by numerical modeling results.
Zhang et al. [48] investigated the evolution of a coastal upwelling event in the southern TWS using intensive cruise data and satellite data in summer 2004; the upwelling-related surface cold water was observed near Dongshan in early July, which then reduced its size by half with a decreased Chl-a concentration after half a month, and eventually vanished by the end of July.
As reviewed by Hong and Wang [49], Shang et al. [50], and Hong et al. [51], the TWS upwelling exhibits clear connections to the ENSO, global climate change, and local environmental variation.
Hu et al. [52] showed that two upwelling-related low temperature (high salinity) regions in the western TWS have clear interannual and intermonthly variability in summer. Combining SST and Chl-a data, Shang et al. [53, 54, 55] proposed that the ENSO events can potentially have significant impacts on the upwelling in the TWS. Tang et al. [56] revealed interannual variation of two upwelling zones (one near Dongshan) in the southern TWS. These studies indicated that the coastal upwelling in the western TWS has evident connections to the ENSO events. The local wind is much weaker in the TWS during the 1997 El Niño year than that during the 1998 La Niña year [57], suggesting that the ENSO event can affect the wind pattern over the TWS and thus modulate the surface ocean currents, SST, and coastal upwelling in an interannual scale. Hong et al. [46] further revealed that, for the entire western TWS, the summer coastal upwelling was strong in 1987, 1993, and 1998 (Figure 5), during which periods three peaks of the SST Empirical Orthogonal Function Mode 1 (EOF_1) time series matched well, with a time lag of 3 months, with those of the multivariate ENSO index (MEI).
Variation of the eigenvector of SST EOF Mode 1 (EOF_1) in the TWS (black dots) and monthly multivariate ENSO index (MEI; shaded areas) 3 months ahead of the SST EOF_1 eigenvector during 1985–2005. The SST EOF_1 eigenvector is normalized by its maximum for the period 1985–2005. Redrawn from Hong et al. [46].
By comparing remote sensing SST with in situ chemical and biological data collected since 1985, Hong et al. [58] obtained evidence of upwelling variation in response to interannual environmental variability in the TWS. According to these observations, the coastal upwelling was weakened in summer of 1997, resulting in an apparent anomaly in nutrient distribution, phytoplankton and zooplankton abundances, and community structure. Hong et al. [51] further summarized the hydrographical features with an emphasis on upwelling, which is the key driver of biogeochemical processes and ecosystem dynamics in the TWS. Hydrographic and satellite data revealed evident teleconnections between the TWS upwelling and the ENSO variability. Besides, Wang et al. [59] estimated the physical (i.e., coastal upwelling) and biological effects on the nutrient transport in the TWS during summer through a coupled physical-biological numerical ocean model. These studies concluded that the TWS upwelling has a profound impact on biogeochemical processes, biological productivity, and ecosystem structure.
Several numerical models, such as a 3D nonlinear baroclinic shallow water model [60, 61, 62], the Coupled Hydrodynamical-Ecological Model for Regional and Shelf Seas (COHERENS; [63]) model [64], and a 3D nonlinear Estuarine, Coastal and Ocean Modeling System with Sediment (ECOMSED) model [65], have been used to study the mechanism of upwelling along the coasts of Fujian and Zhejiang in summer and winter. These numerical modeling results indicated that the wind stress, the Taiwan Warm Current, tidal nonlinear effect, and bottom topography are the main mechanisms for the upwelling in the coastal waters of Fujian and Zhejiang in both winter and summer. Specifically, the southwesterly or southerly wind induces the coastal upwelling in summer.
Furthermore, Jiang et al. [66] investigated the mechanisms of coastal upwelling in the southern TWS using a nested circulation model based on the POM. It is indicated that the upslope current over a distinctly widened shelf transports the cold water toward the shore in the lower layer, while the southwesterly monsoon wind drives the cold water away from the shore in the surface layer, thus generating the upwelling along the southwestern coast of the TWS.
The studies of coastal upwelling in the ECS have been conducted using hydrographic measurements, satellite observations, and numerical modelling. For recent decades, much progress of the upwelling study has been made particularly in the quick developments of numerical modelling technology and remote sensing approach.
Zhao et al. [67] reported an upwelling north of the Yangtze River (or the Changjiang River) Estuary, covering an area of roughly 1° by 1° centered at (31°30′N, 122°40′E). Several cruise measurements, such as the China-Korea joint investigation in the Yellow Sea and its adjacent sea area [68] and the marine flux investigation in the ECS in July 1998 [69], confirmed the existence of this upwelling in the Yangtze River Estuary. Zhu et al. [70] analyzed the hydrological characteristics in the outer Yangtze River Estuary and showed that the upwelling usually occurs near the first turning point of the Yangtze River Diluted Water. Zhu et al. [71] conducted comprehensive observations in August 2000 and indicated that the coastal upwelling appears along the Zhejiang coast, in the west of the submarine river valley and along the Lüsi coast. Lü et al. [72] presented signals of low-temperature and high-salinity upwelling water in the Yangtze River Estuary using three sections of temperature and salinity distributions (Figure 6) obtained from a cruise in August 2000. There is evidence that in the Yangtze River Estuary the subsurface high-salinity water can rise toward the 5–10 m layer from beneath.
Vertical distributions of temperature (°C; left panels) and salinity (right panels) along Section 32.0°N (top), Section 31.5°N (middle), and Section 31.0°N in the Yangtze River Estuary. Redrawn from Lü et al. [72].
Hu and Zhao [73] studied the long-term variation of coastal upwelling off northeastern Zhejiang in summer using SST (1987–2005), Chl-a (2002–2006), and wind (1992–2006) datasets; their results showed that the upwelling, with high Chl-a concentration, has seasonal, annual, and interannual variations. Hu and Zhao [74] investigated the short-term varia-tion of upwelling in the Zhejiang coastal areas during May–October 2004 and indicated that the upwelling has a close relation to the along-shore wind variation. Lou et al. [75] depicted the evolution of the upwelling along Zhejiang coast, which appears in June, peaks in July and August, and then diminishes until disappears in late September. The mean SST in the upwelling region is about 25-28°C in summer, with a temperature difference of approximately 2–4°C from the ambient nonupwelling waters. Cao et al. [76] investigated the summertime upwelling off the Yangtze River Estuary using satellite data and proposed that along-shore wind stress and wind stress curl play similar important roles on the upwelling evolution.
Numerical models have been developed or applied for studying the characteristics of coastal upwelling and its dynamics in the ECS (Table 1). These simulations suggested that the coastal upwelling usually appears off the Yangtze River Estuary and along the Zhejiang coast, mostly in summer. The continental slope, wind speed, and the angle between the wind direction and the coastline control the coastal upwelling intensity. Topography, Yangtze River discharge, the Taiwan Warm Current, and the branch current bifurcating from the subsurface of the Kuroshio all affect the upwelling. In addition, baroclinic (barotropic) effect is the main factor for inducing upwelling in the north (south) of submarine river valley off the Yangtze River Estuary [77]. However, in the coastal waters near the Zhoushan Islands (located off the northeastern coast of Zhejiang), wind forcing may sometimes exert negative influences on the generation of coastal upwelling by weakening the intrusion of the Taiwan Warm Current onto the continental shelf [72].
Authors | Model | Features |
---|---|---|
Li and Zhao [78] | POM | Upwelling phenomena in the Yangtze River Estuary. |
Zhao et al. [79] | POM | Upwelling mechanism in the Yangtze River Estuary. |
Zhu [77] | 3D numerical model | Baroclinic (barotropic) effect is the main factor for inducing upwelling in the north (south) of submarine river valley off the Yangtze River Estuary. |
Bai and Wang [80] | POM | Upwelling occurs around 10 km away from the coastline in the Yangtze River Estuary. |
Liu et al. [81] | 3D baroclinic ocean model | Seasonal variation of the vertical circulation in the ECS. |
Liu et al. [82] | 3D baroclinic ocean model | Temperature and salinity features are associated with upwelling or downwelling. |
Zhu et al. [83] | ECOM-si model (ECOM with semi implicit scheme) | Upwelling is mainly the baroclinic effect induced by mixing between the fresh water from the Yangtze River and the saline water offshore. |
Qiao et al. [84] | MASNUM | Owing to a strong density gradient, the baroclinic pressure gradient force is large near the frontal zone, which elicits an upwelling branch along the topographic slope. |
Lü et al. [72] | MASNUM | Upwelling is induced as a branch of the secondary circulation. Topography, Yangtze River discharge, and the Taiwan Warm Current all affect the upwelling. |
Jing et al. [85] | ECOMSED model | Upwelling occurs along the coasts of Zhejiang and Fujian throughout the year, which is strong in summer and relatively weak in winter. |
Lü et al. [86] | MASNUM | Tides (barotropic and baroclinic processes) are key to the upwelling off the Yangtze River Estuary. |
Bai et al. [87] | ECOMSED model | Upwelling is mainly induced by the Ekman effect and affected by the Taiwan Warm Current and continental slope rising. |
Yang et al. [88] | ROMS | A branch current bifurcates from the subsurface of the Kuroshio northeast of Taiwan, upwells northwestward, then turns to northeast around (27.5oN, 122°E), and finally reaches 31°N off the Yangtze River mouth. |
Cao et al. [76] | ROMS | Wind primarily influences the short-term evolution of upwelling, while the topographic variation determines the upwelling center off the Yangtze River Estuary. |
Liu and Gan [89] | 3D high-resolution numerical model | Intensified upwelling is formed by a strengthened shoreward transport downstream of the promontory coastline. |
Yang et al. [90] | ROMS coupled with phosphate model | The transported phosphate-rich water is further upwelled to the surface due to the upwelling just off the Zhejiang coast. |
Numerical models used in studying the upwelling in the ECS.
Note: MASNUM is a model established by the Laboratory of MArine Sciences and NUmerical Modeling, the State Oceanic Administration, China.
As mentioned above, the influence of topography on the generation and modulation of coastal upwelling has been observed in the ECS, TWS, and the northern SCS; so it is worthy of being separately discussed here as an important upwelling-related factor. A 3D modelling study by Gan et al. [91] revealed that the widened shelf off Shantou plays an important role in intensifying the local upwelling. The strongest advection occurs over the converging isobaths near Shanwei, i.e., the head of the widened shelf (Figure 7) where a negative pressure gradient also exists at the lee of the coastal cape over the inner shelf and locally amplifies shoreward motion. In addition, Chen [92] discussed the effects of cape and canyon on wind-driven coastal upwelling in the western TWS, suggesting that the positive vertical velocity is produced by changes in the relative vorticity downstream of the cape or canyon, which becomes a dominant upwelling mechanism there. Topography also exerts influences on upwelling by steering bottom currents upward. Upwelling can even be intensified by a strengthened shoreward transport downstream of a promontory coastline [89]. Recently, Wang et al. [93] investigated relative contributions of the local wind and topography to the coastal upwelling intensity in the northern SCS in the case when the upwelling-favorable wind retreats, using a high-resolution version of the POM. It is indicated that the topographically induced upwelling is comparable with the wind-driven upwelling at surface; while at bottom, topography has a stronger contribution than the local wind in controlling the upwelling intensity in the inner shelf of the northern SCS [93].
Schematic picture showing the wind-driven upwelling processes and forcing mechanism over the middle and inner shelves of a widened shelf. Redrawn from Gan et al. [91]. PGF denotes pressure gradient force; UAD and UBC are mean velocities normal to the two streamlines AD and BC, respectively. The line AD is at the head of the widened shelf (near Shanwei) and BC, downstream of it (near Shantou).
For the upwelling near the Pearl River Estuary, the interaction between upwelling and river plume should be considered [94, 95, 96]. The enhanced stratification due to the presence of plume thins the surface frictional layer and strengthens the cross-shelf circulation in the upper water column. As a result, the surface Ekman current and the compensating flow beneath the plume are amplified, while the shoaling of the deeper dense water minimally changes in the upwelling region. The pressure gradient generated between the buoyant plume and the ambient sea water accelerates the wind-driven current along the inshore edge of the plume, but retards it along the offshore edge [95]. The buoyancy in the plume considerably modulates the alongshore and cross-shelf upwelling circulation in the upper water column [95], and that the upwelling initially occurs to the east of the Pearl River Estuary, intensifies eastward, and reaches its maximum near Shantou [96]. For the upwelling off the Yangtze River Estuary area, upwelling is associated with a strong salt-induced horizontal density gradient. The plume fronts separate the diluted and saline water, and this density structure elicits upwelling as a branch of the density-driven secondary circulation [72].
The density (or salinity) front, which separates the inshore low-salinity coastal water from the offshore Taiwan Warm Current Water, is one of the primary inducing factors for the upwelling along the western coast of ECS. Using a numerical model, Yang et al. [88] revealed that the upwelling off the Zhejiang coast comes from the subsurface water of the Kuroshio northeast of Taiwan in summer (Figure 8). The phosphate-rich upwelling water off the coast of Zhejiang is mainly originated from the deep sea water in a special area (122.1°E–122.5°E, 130 m–300 m deep) northeast of Taiwan, as the nearshore Kuroshio branch current continuously transports the phosphate-rich deep sea water to the bottom area off the coast of Zhejiang [90].
Summer ocean circulation pattern in the ECS. The solid thin lines represent the isobaths of 50, 100, and 1000 m. The bold dashed line represents the possible ocean current of the Kuroshio Bottom Branch Current to the northeast of Taiwan (KBBCNT). The bold solid lines show the Kuroshio, the Kuroshio Branch Current (KBC), and the Taiwan Warm Current (TWC), and UW denotes upwelling. Redrawn from Yang et al. [88].
As for the northern SCS, Wang et al. [97] investigated the subsurface upwelling signals off the coasts of Fujian and Guangdong provinces in summer 2000, using a combination of hydrographical, tide-gauge and mooring data, satellite observations, and numerical circulation model output. It is suggested that the subsurface upwelling is closely related to the coastal sea level fluctuation and is evidently modulated by both local wind-forcing and large-scale SCS circulation.
Lü et al. [98] studied the summertime upwelling off the western coast of Hainan Island using satellite SST data and numerical modeling. The presence of the tidal mixing front [99] was believed to play a profound role in stimulating the upwelling near the southwestern coast of Hainan Island. This upwelling was also evidenced by comprehensive cruise data collected in the summer of 2006 [100]. On the other hand, the southwesterly monsoon induces downwelling that competes with the front-induced upwelling off the western coast of Hainan Island.
In the TWS and the ECS, Hong et al. [101] also indicated that tidal mixing plays important roles in enhancing the upwelling in the TWS. In addition, tides contribute to the upwelling generation because tidal mixing facilitates the expansion of the Yangtze River Diluted Water, and strong tidal mixing results in considerable horizontal density gradient across a tidal front and thus induces upwelling [72, 86].
Internal tides may also affect the upwelling intensity [102, 103]. These studies used satellite multisensor data such as the moderate resolution imaging spectroradiometer (MODIS) SST, QuikSCAT ocean surface winds, and sea surface dynamic height, and suggested that the interaction between upwelling and internal tides enhances the uplifting of lower-layer water; thus, the summertime upwelling pattern and intensity tend to be altered on the shelf off Guangdong.
There are six major coastal upwelling regions off the southeastern coast of mainland China, as shown in Figure 2. The main features of these coastal upwelling regions are summarized below.
In the northern SCS, coastal upwelling regions are distributed primarily off the eastern coast of Hainan Island and off the coasts of eastern Guangdong. The southwesterly monsoonal winds are the most prominent factor controlling the upwelling generation. Besides the alongshore wind stress, wind stress curl, distinct topographic features, frontal eddies, and local circulations are among the mechanisms for the coastal upwelling in the northern SCS.
In the TWS, two main coastal upwelling regions are identified, i.e., along the southwestern and northwestern coasts of the TWS. The former appears between Xiamen and Shantou, while the latter occurs from the east of Pingtan to Meizhou. Both upwellings are regarded as wind-driven, which occur during the southwesterly monsoon period with a relatively strong intensity in July. In addition, the bottom topography and the ascending of the northward current also affect the upwelling. With respect to the time-varying features, the coastal upwelling in the western TWS shows short-term variations caused by winds, and has evident responses to ENSO or local environmental variations.
In the ECS, coastal upwellings are observed in the Yangtze River Estuary and along the coast off Zhejiang. The alongshore wind, topography, tides, and local circulation are among the significant factors in determining the generation of coastal upwellings.
Upwelling in the coastal waters of China seas is complex, in terms of the spatial distribution, time-varying characteristics, generation mechanisms, and factors affecting its evolution and dynamics. It covers a wide range of temporal variability, including interannual and multidecadal timescales associated with the ENSO events and global climate change, as well as shorter timescales associated with fluctuations caused by winds or internal tides. Consequently, observations based solely on limited cruise measurements would not be able to provide in-depth knowledge of the upwelling dynamics or its associated biogeochemical processes. A number of dedicated offshore surveys covering all seasons have been conducted in the China seas over 2005–2011, aiming with a constant goal of collecting more hydrographic data as well as biogeochemical parameters. A much better understanding of the main characteristics and dynamics of upwelling in the China seas has been gained, based on these in situ measurements, multisources of satellite remote sensing data and outputs from global/regional ocean circulation models (some with biogeochemical modules) [104, 105]. Nevertheless, there are still certain issues related to coastal upwelling, which remain to be addressed in the near future, for example, the possible changes of upwelling under global climate change, the influences of submesoscale processes on the upper-ocean upwelling, etc.
This work is jointly supported by the National Basic Research Program of China (2015CB954004) and the National Natural Science Foundation of China (41776027, 41606009 and U1405233).
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