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Increased frequency of extreme Indian Ocean Dipole events due to greenhouse warming

机译:由于温室气候变暖,印度洋偶极子极端事件发生的频率增加

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摘要

The Indian Ocean dipole is a prominent mode of coupled ocean-atmosphere variability, affecting the lives of millions of people in Indian Ocean rim countries. In its positive phase, sea surface temperatures are lower than normal off the Sumatra-Java coast, but higher in the western tropical Indian Ocean. During the extreme positive-IOD (pIOD) events of 1961, 1994 and 1997, the eastern cooling strengthened and extended westward along the equatorial Indian Ocean through strong reversal of both the mean westerly winds and the associated eastward-flowing upper ocean currents. This created anomalously dry conditions from the eastern to the central Indian Ocean along the Equator and atmospheric convergence farther west, leading to catastrophic floods in eastern tropical African countries but devastating droughts in eastern Indian Ocean rim countries. Despite these serious consequences, the response of pIOD events to greenhouse warming is unknown. Here, using an ensemble of climate models forced by a scenario of high greenhouse gas emissions (Representative Concentration Pathway 8.5), we project that the frequency of extreme pIOD events will increase by almost a factor of three, from one event every 17.3 years over the twentieth century to one event every 6.3 years over the twenty-first century. We find that a mean state change-with weakening ofboth equatorial westerly winds and eastward oceanic currents in association with a faster warming in the western than the eastern equatorial Indian Ocean-facilitates more frequent occurrences of wind and oceanic current reversal. This leads to more frequent extreme pIOD events, suggesting an increasing frequency of extreme climate and weather events in regions affected by the pIOD.%南热带印度洋地区的国家在"印度洋偶极子"(IOD)气候周期处于一个极端正阶段的年份中易发生大范围洪涝和旱灾。在这些"坏年份"(如1961、1994和1997年)中,温暖水域会出现在印度洋海盆的西部,降水量会増加;而在东部则主要是较冷水域,降水量会减少。在这篇论文中,Wenju Cai等人对在高温室气体排放情景下的气候模型预测结果进行了评估,发现极端正IOD的出现频率在21世纪可能会从整个20世纪的每17.3年大约一次増加到每6.3年一次。
机译:印度洋偶极子是海洋-大气可变性的一种突出模式,它影响着印度洋边缘国家数百万人的生活。在其积极阶段,苏门答腊爪哇海岸的海面温度低于正常水平,但在热带西印度洋则较高。在1961年,1994年和1997年的极端IOD事件中,通过平均逆风和相关的向东流动的上层洋流的强烈逆转,东部冷却作用增强并沿赤道印度洋向西扩展。这从赤道东部到中部印度洋沿赤道创造了异常干燥的条件,更西端的大气汇聚,导致东部热带非洲国家发生灾难性洪灾,但破坏了东部印度洋边缘国家的干旱。尽管有这些严重的后果,但pIOD事件对温室变暖的响应仍然未知。在这里,使用由高温室气体排放引起的气候模型集合(代表浓度路径8.5),我们预测极端pIOD事件的发生频率将增加近三倍,而在过去的17.3年中每发生1次二十世纪到二十一世纪每6.3年发生一次事件。我们发现,平均状态变化-赤道西风和东洋海流减弱,同时西部的变暖要比东部赤道印度洋更快,这促使风和洋流逆转的发生更加频繁。这导致更频繁的极端pIOD事件发生,这表明受pIOD影响的地区中极端气候和天气事件的频率增加。%南热带印度洋地区的国家在“印度洋偶极子”(IOD)在这些“坏年份”(如1961、1994和1997年)中,温暖的水域会出现在印度洋海盆的西部,必然量会増加;而在东部则主要是较旧的在介绍论文中,Wenju Cai等人对在高温室气体排放情景下的气候模型预测结果进行了评估,发现极端正IOD的出现频率在21世纪可能会从整个20世纪的每17。3年大约一次増加到每6。3年一次。

著录项

  • 来源
    《Nature》 |2014年第7504期|254-258B1|共6页
  • 作者单位

    CSIRO Marine and Atmospheric Research, Aspendale, Victoria, 3195 Australia,Physical Oceanography Laboratory, Qingdao Collaborative Innovation Center of Marine Science and Technology, Ocean University of China, Qingdao, 266003 China;

    Climate Change Research Centre and ARC Centre of Excellence for Climate System Science, The University of New South Wales, Sydney, 2052 Australia;

    Physical Oceanography Laboratory, Qingdao Collaborative Innovation Center of Marine Science and Technology, Ocean University of China, Qingdao, 266003 China,CSIRO Marine and Atmospheric Research, Aspendale, Victoria, 3195 Australia;

    CSIRO Marine and Atmospheric Research, Aspendale, Victoria, 3195 Australia;

    Physical Oceanography Laboratory, Qingdao Collaborative Innovation Center of Marine Science and Technology, Ocean University of China, Qingdao, 266003 China;

    Centre for Climate Change Research, Indian Institute of Tropical Meteorology Pashan, Pune 411 008, India;

    Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo 113-0033, Japan,Climate Variation Predictability and Applicatability Research Program, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), 3173-25 Showa-machi, Kanazawa-ku, Yokohama 236-0001, Japan;

    Application Laboratory, JAMSTEC, 3173-25 Showa-machi, Kanazawa-ku, Yokohama 236-0001, Japan;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
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