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Short-term Climate Characteristics at Ny-Alesund over the Arctic Tundra Area

机译:北极苔原地区新奥勒松的短期气候特征

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摘要

Based on the Germany Koldwey Station's 1994-2003 conventional observation hourly data, this paper conducts a statistical analysis on the short-term climate characteristics for an arctic tundra region (Ny-Alesund island) where our first arctic expedition station (Huanghe Station) was located. Affected by the North Atlantic warming current, this area has a humid temperate climate, and the air temperature at Ny-Alesund rose above 0℃ even during deep winter season during our research period. The wind speed in this area was low and appeared most at southeast direction. We find that the temperature at Ny-Alesund rose in the faster rate (0.68℃/10 a) than those at the whole Arctic area. Compared with the floating ices where our expedition conducted in the Arctic, Ny-Alesund was warmer and more humid and had lower wind speed. Comparison of the near surface air temperature derived by NCEP/NCAR reanalysis to the conventional measurements conducted at the Koldwey site in Ny-Alesund area shows a good a-greement for winter season and a significant difference for summer season.
机译:基于德国Koldwey站1994-2003年的常规观测小时数据,本文对第一个北极探险站(黄河站)所在的北极苔原地区(Ny-Alesund岛)的短期气候特征进行了统计分析。 。受北大西洋变暖影响,该地区属温带湿润气候,在本研究期间,即使在深冬季,Ny-Alesund的气温也上升至0℃以上。该地区的风速低,并且在东南方向最多出现。我们发现,Ny-Alesund的温度上升速度比整个北极地区的上升速度快(0.68℃/ 10 a)。与我们在北极进行的考察中的浮冰相比,新奥勒松更温暖,更潮湿并且风速更低。通过NCEP / NCAR再分析得出的近地表空气温度与在Ny-Alesund地区的Koldwey站点进行的常规测量结果的比较表明,冬季是一个很好的协议,而夏季则存在显着差异。

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