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Intensification and deepening of the Arabian Sea oxygen minimum zone in response to increase in Indian monsoon wind intensity

机译:阿拉伯海氧气最小区域的强化和深化响应印度季风风强度的增加

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The decline in oxygen supply to the ocean associated with global warming is expected to expand oxygen minimum zones (OMZs). This global trend can be attenuated or amplified by regional processes. In the Arabian Sea, the world's thickest OMZ is highly vulnerable to changes in the Indian monsoon wind. Evidence from paleorecords and future climate projections indicates strong variations of the Indian monsoon wind intensity over climatic timescales. Yet, the response of the OMZ to these wind changes remains poorly understood and its amplitude and timescale unexplored. Here, we investigate the impacts of perturbations in Indian monsoon wind intensity (from 50 to +50 %) on the size and intensity of the Arabian Sea OMZ, and examine the biogeochemical and ecological implications of these changes. To this end, we conducted a series of eddy-resolving simulations of the Arabian Sea using the Regional Ocean Modeling System (ROMS) coupled to a nitrogen-based nutrient-phytoplankton-zooplankton-detritus (NPZD) ecosystem model that includes a representation of the O-2 cycle. We show that the Arabian Sea productivity increases and its OMZ expands and deepens in response to monsoon wind intensification. These responses are dominated by the perturbation of the summer monsoon wind, whereas the changes in the winter monsoon wind play a secondary role. While the productivity responds quickly and nearly linearly to wind increase (i.e., on a timescale of years), the OMZ response is much slower (i.e., a timescale of decades). Our analysis reveals that the OMZ expansion at depth is driven by increased oxygen biological consumption, whereas its surface weakening is induced by increased ventilation. The enhanced ventilation favors episodic intrusions of oxic waters in the lower epipelagic zone (100-200 m) of the western and central Arabian Sea, leading to intermittent expansions of marine habitats and a more frequent alternation of hypoxic and oxic conditions there. The increased productivity
机译:与全球变暖相关的海洋氧气供应减少预计将扩大氧气最低区(OMZ)。这种全球趋势可以通过区域进程减弱或放大。在阿拉伯海,世界上最厚的OMZ极易受到印度季风变化的影响。来自古记录和未来气候预测的证据表明,印度季风风力强度在气候时间尺度上有很大的变化。然而,OMZ对这些风变化的响应仍知之甚少,其振幅和时间尺度尚未探索。在这里,我们研究了印度季风风强度(从50%到+50%)扰动对阿拉伯海OMZ大小和强度的影响,并研究了这些变化的生物地球化学和生态影响。为此,我们使用区域海洋建模系统(ROMS)和氮基营养浮游植物浮游动物碎屑(NPZD)生态系统模型对阿拉伯海进行了一系列涡分解模拟,该模型包括O-2循环的表示。我们表明,阿拉伯海生产力增加,其OMZ随着季风的增强而扩大和加深。这些响应主要受夏季风扰动的影响,而冬季风的变化起次要作用。虽然生产力对风力增加的响应速度很快,几乎呈线性(即在数年的时间尺度上),但OMZ的响应速度要慢得多(即在数十年的时间尺度上)。我们的分析表明,OMZ在深度的扩张是由增加的氧气生物消耗驱动的,而其表面弱化是由增加的通风引起的。增强的通风有利于阿拉伯海西部和中部下部表层带(100-200 m)有毒水域的间歇性侵入,导致海洋栖息地的间歇性扩张,以及那里缺氧和有毒条件的更频繁交替。生产力的提高

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