Characteristics of Marine Heat Extreme Evolution in the Northern Indian Ocean

IF 3.5 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Hitesh Gupta, Rahul Deogharia, Sourav Sil, Dipanjan Dey
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引用次数: 0

Abstract

Marine Heat Extremes (MHEs) are events of anomalously high Sea Surface Temperature (SST) during which SST values exceed a certain pre-defined threshold. These MHEs have profound influence over weather patterns, air-sea interaction and the health of marine ecosystems. This study investigates the long-term evolution of MHEs in the Northern Indian Ocean (NIO) from 1900 to 2020. We utilised two normalised indices, the Normalised Extreme Frequency Index (NEFI) for frequency and the Normalised Extreme Heat Index (NEHI) for the intensity of MHEs, to objectively compare the MHE attributes across different periods and regions of the NIO. The analysis reveals non-linearly increasing NEFI, with the Western Equatorial Indian Ocean (WEIO) experiencing the fastest rise, followed by the Eastern Equatorial Indian Ocean (EEIO), Arabian Sea (AS) and Bay of Bengal (BoB). MHE intensity shows exponential growth, with its mean-based regimes becoming shorter and shifting more frequently. A new regime has been emerging since the last decade. Analysis of the spatial extent of the MHEs indicates that the WEIO is the fastest-growing region of the NIO. Similar observations were found upon removing sub-decadal variabilities, which include the potential effects of El Niño-Southern Oscillation and Indian Ocean Dipole, highlighting the long-term warming associated with global warming. The study also links the increasing mean SST to the rising frequency and intensity of MHEs, which is predominantly driven by the net surface heat-flux, which is a combined effect of local and pantropical air-sea interaction. The surface warming is outpacing subsurface warming, thereby strengthening thermal stratification over time, potentially impacting vertical mixing and upwelling, which can, in turn, lead to further surface warming.

北印度洋海洋热极端演化特征
海洋极端高温(MHEs)是指海表温度(SST)异常高且超过特定阈值的事件。这些MHEs对天气模式、海气相互作用和海洋生态系统的健康有着深远的影响。本文研究了1900 - 2020年北印度洋MHEs的长期演变。我们利用两个标准化指数,即标准化极端频率指数(NEFI)的频率和标准化极端热指数(NEHI)的强度,客观地比较了NIO不同时期和不同地区的MHE属性。NEFI呈非线性增长,其中西赤道印度洋(WEIO)上升最快,其次是东赤道印度洋(EEIO)、阿拉伯海(AS)和孟加拉湾(BoB)。MHE强度呈指数增长,其基于均值的机制变得更短,变化更频繁。自上个十年以来,一种新的体制已经出现。对MHEs的空间范围分析表明,WEIO是NIO增长最快的区域。在去除次年代际变化(包括El Niño-Southern涛动和印度洋偶极子的潜在影响)后,发现了类似的观测结果,突出了与全球变暖相关的长期变暖。该研究还将平均海温的增加与MHEs频率和强度的增加联系起来,MHEs主要是由净地表热通量驱动的,而净地表热通量是局地和泛热带海气相互作用的综合效应。地表变暖的速度超过了地下变暖,从而随着时间的推移加强了热分层,潜在地影响了垂直混合和上升流,这反过来又可能导致地表进一步变暖。
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来源期刊
International Journal of Climatology
International Journal of Climatology 地学-气象与大气科学
CiteScore
7.50
自引率
7.70%
发文量
417
审稿时长
4 months
期刊介绍: The International Journal of Climatology aims to span the well established but rapidly growing field of climatology, through the publication of research papers, short communications, major reviews of progress and reviews of new books and reports in the area of climate science. The Journal’s main role is to stimulate and report research in climatology, from the expansive fields of the atmospheric, biophysical, engineering and social sciences. Coverage includes: Climate system science; Local to global scale climate observations and modelling; Seasonal to interannual climate prediction; Climatic variability and climate change; Synoptic, dynamic and urban climatology, hydroclimatology, human bioclimatology, ecoclimatology, dendroclimatology, palaeoclimatology, marine climatology and atmosphere-ocean interactions; Application of climatological knowledge to environmental assessment and management and economic production; Climate and society interactions
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