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Air temperature changes in the Arctic in the period 1951-2015 in the light of observational and reanalysis data

机译:根据观测和再分析数据,北极在1951-2015年期间的气温变化

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摘要

Recent air temperature changes in the high Arctic (HA) have been investigated based on mean seasonal and annual data calculated for the period 1951-2015 and for two sub-periods 1976-2015 and 1996-2015. Two kinds of air temperature data (observational and reanalysis) have been used in the research. The observational data were compared with data taken from six reanalysis products (20CRv2c, CERA-20C, ERA-Int, MERRA-2, NCEP-CFSRR, JRA-55). The scale of the HA warming for the period 1996-2015 relative to the reference period 1951-1990 reached 1.6 degrees C for annual mean and was greatest in autumn (1.9 degrees C) and in winter (1.7 degrees C), while it was smallest in summer (0.9 degrees C). Evidently, the greatest warming was observed in the Atlantic and Siberian climatic regions, while in the rest of the HA, the rate of warming was usually weaker than trends calculated for the period 1976-2015. Air temperature tendencies in all study periods 1951-2015, 1976-2015 and 1996-2015 showed a predominance of positive trends that were statistically significant at the level of 0.05. In the two latter periods, the rate of warming was on average 2-3 times faster than for the entire study period. In the HA, there has not been a slowdown in the rate of warming ("hiatus") in the last two decades (in contrast to that which was noted for the Northern Hemisphere). Our results reveal that, in most cases, the closest fit to observations was obtained for two reanalysis products (the ERA-Interim and JRA-55, since 1979) and the six reanalysis average. Two new polar amplification (PA) metrics based on scaled and standardised values of surface air temperature (SAT) reveal the non-existence of this phenomenon in the period 1951-2015. One of the metrics shows very small PA in the periods 1976-2015 and 1996-2015.
机译:根据1951-2015年期间以及两个1976-2015年和1996-2015年两个子时期的平均季节和年度数据,对北极地区(HA)的近期气温变化进行了调查。研究中使用了两种空气温度数据(观测和再分析)。将观测数据与六种再分析产品(20CRv2c,CERA-20C,ERA-Int,MERRA-2,NCEP-CFSRR,JRA-55)的数据进行比较。相对于参考时期1951-1990年,HA的变暖规模为1996-2015年,年均达到1.6摄氏度,秋季(1.9摄氏度)和冬季(1.7摄氏度)最大,而最小在夏季(0.9摄氏度)。显然,在大西洋和西伯利亚气候区域观察到最大的变暖,而在高可用性的其余部分,变暖速度通常弱于1976-2015年期间的趋势。在1951-2015年,1976-2015年和1996-2015年的所有研究期间,气温趋势均显示出积极趋势,这些趋势在0.05的水平上具有统计学意义。在后两个时期,升温速度平均比整个研究时期快2-3倍。在医管局中,最近二十年来,升温(“裂口”)没有减慢(与北半球的情况相反)。我们的结果表明,在大多数情况下,两种再分析产品(ERA-Interim和JRA-55,自1979年以来)和六个再分析平均值均与观测值最接近。基于地表气温(SAT)的标定和标准化值的两个新的极地放大(PA)指标揭示了这一现象在1951-2015年间不存在。其中一项指标显示,1976-2015年和1996-2015年期间的PA很小。

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