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不同再分析气温在东南极中山站-DomeA断面的适用性评价

DOI: 10.1007/s11430-013-4684-4, PP. 156-168

Keywords: 东南极,再分析资料,表层气温,中山站-DomeA,自动气象站

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Abstract:

?对比分析2005~2008年五种再分析资料和东南极地区气象站实测的日平均2m气温,结果表明:五种再分析资料都能够解释超过70%的方差,年均方根误差为3.4~6.9℃.三种NOAA再分析资料NCEP-1,NCEP-2和20CRv2呈现冷偏差(分别为-2.5,-1.4和-1.5℃),ERAInterim和JCDAS呈现暖偏差(分别为1.7和2.0℃).五种再分析气温通常在(南半球)春季适用性强,冬、秋季适用性差;在海拔2800m高原内陆EAGLE地区适用性最强,在东南极冰盖最高点DomeA地区适用性最差.ERAInterim适用性优于其他再分析资料,可能源于其4D同化体系;三种NOAA再分析资料适用性最差,因为其同化体系更多地受控于有限的观测资料,20CRv2同化数据更少,仅仅同化了表面气压观测资料.虽然再分析气温具有一定的不足和局限性,但是,仍然不失为南极地区气候研究的有效工具.在南极,尤其是在广袤的南极内陆地区,进一步加强更多的实地观测显得尤为重要.

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