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Global Warming, Atlantic Multi-decadal Oscillation, Thermohaline Catastrophe and Their Impact on Climate of the North Atlantic Region

机译:全球变暖,大西洋多层振荡,热河灾害灾难及其对北大西洋地区气候的影响

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This paper presents investigation of regional and global warming, Atlantic Multidecadal Oscillation (quasiperiodic natural variations of the ocean-atmosphere system in the North Atlantic with typical time scales of 50-100 years) and thermohaline catastrophe (blocking of thermohaline circulation in the North Atlantic). The typical scale of the Atlantic Multidecadal Oscillation (AMO) is determined by the intensity of the meridional oceanic circulation in the North Atlantic. The analyzed oscillation affects various climatic characteristics: air temperature, river discharge in the European and North-American regions, the number and intensity of tropical cyclones in the Atlantic Ocean, and the parameters of mid-latitude cyclones and anticyclones in the Atlantic-European region. The main mechanism by which the AMO affects the climatic characteristics of the regions neighboring with the North Atlantic is the atmospheric response to the thermal anomalies in the ocean leading to a shift of the centers of atmospheric action and to the changes in the intensity and predominant directions of propagation of atmospheric cyclones and anticyclones. By using the results of long-term instrumental observations carried out in Eastern Europe and the data array of reconstructed temperature in the Alpine region, it is shown that the AMO is responsible for a significant part of low-frequency variations of temperature in Europe. This fact confirms the potential predictability of the regional atmospheric AMO on the decadal-scale. The rate of quasi-periodical regional warming/cooling of surface air temperature due to AMO can exceed the regional temperature rising due to global warming. So, the fast warming of the North Atlantic region during the last 3-4 decades of the twentieth century is due to coincidence of human-induced temperature increase and transition from negative to positive phase of the AMO. Realization of thermohaline catastrophe for the recent climatic epoch is unlikely.
机译:本文呈现区域性和全球变暖的调查,大西洋Multidecadal涛动(海洋 - 大气系统在北大西洋的50 - 100年的典型时间尺度的准周期自然变化)和温盐灾难(北大西洋阻塞温盐环流) 。大西洋Multidecadal振荡(AMO)的典型比例是通过在北大西洋子午海洋环流的强度来确定。该分析振动影响各种气候特点:气温,在欧洲和北美地区,在大西洋热带气旋的数量和强度河流流量,旋风和反气旋在大西洋欧洲区中纬度的参数。通过该AMO影响与北大西洋周边地区的气候特征的主要机制是在海洋中的热异常导致大气活动的中心的转变,在强度和主要方向变化的大气响应的大气气旋和反气旋的传播。通过使用在东欧和在高寒地区重构温度的数据阵列进行长期仪器观察结果中,示出的是,AMO是负责在欧洲温度的低频变化的显著一部分。这一事实印证了区域大气AMO上的年代际尺度的潜力可预测性。准周期性区域变暖/速率由于AMO冷却面空气温度可以超过区域温度,由于全球变暖上升。所以,北大西洋地区在过去几十年3-4二十世纪的快速变暖是由于人类活动引起的温度升高和过渡,从消极到AMO的正相巧合。针对近期气候时期温盐灾难的实现是不可能的。

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