首页|基于Aqua卫星AIRS数据的南大洋大气逆温和逆湿特性研究

基于Aqua卫星AIRS数据的南大洋大气逆温和逆湿特性研究

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南大洋大气普遍存在着逆温和逆湿现象,其分布和变化对海-冰-气之间的物质和通量交换具有重要影响。利用Aqua卫星上搭载的大气红外探测器(AIRS)观测数据,提取了南大洋大气的逆温和逆湿特性,并研究了其时空分布与变化特征。此外,以全球无线电探空数据集的探测结果为参考值,分析了AIRS在进行大气逆温和逆湿探测过程中受到云量影响的特征。结果表明,AIRS 估计的逆温特性受云量的影响较小,在多云条件下AIRS也可精确地估计逆温特性。利用AIRS最新的第 7 版(V7)数据产品对 2004-2020 年南大洋大气逆温和逆湿的频率(强度)进行研究,发现秋冬季比春夏季高(强),在龙尼冰架、罗斯冰架和南极半岛附近的海域的大气出现逆温和逆湿现象较其他区域更频繁,且强度更强。
Characteristics of the Southern Ocean temperature and specific humidity in-versions from the Atmospheric Infrared Sounder(AIRS)on the Aqua satellite
The temperature inversion(TI)and specific humidity inversion(SHI)are common over the Southern Ocean,and their distribution and variation have important effects on the exchange of matter and flux be-tween ocean,ice and air.In this study,the TI and SHI characteristics of the Southern Ocean were extracted from data obtained by the Atmospheric Infrared Sounder(AIRS)on the Aqua satellite,and the characteris-tics of their temporal and spatial distributions and variations were studied.In addition,using the sounding results of the Integrated Global Radiosonde Archive 2 as reference values,the effects of cloud in the AIRS TI and SHI estimates were analyzed.The results show that the characteristics of the TI from AIRS data are less affected by clouds,and AIRS can accurately estimate the characteristics of TI under cloudy conditions.The frequency and strength of the TI and SHI over the Southern Ocean from 2004 to 2020 were studied us-ing the latest version of AIRS data(V7).It is found that TI and SHI are higher and stronger in autumn and winter than in spring and summer,and are more frequent and stronger in the Ronne Ice Shelf,Ross Ice Shelf,and the sea area near the Antarctic Peninsula than in other regions.

temperature inversionsspecific humidity inversionsSouthern OceanAqua satelliteAIRS

许妍、常亮、李黎黎

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上海海洋大学海洋科学学院,上海 201306

华象科技(南京)有限公司,江苏 南京 210019

逆温 逆湿 南大洋 Aqua卫星 AIRS

国家自然科学基金面上项目

42174016

2024

极地研究
国家海洋局极地考察办公室 中国极地研究中心

极地研究

CSTPCD北大核心
影响因子:0.638
ISSN:1007-7073
年,卷(期):2024.36(2)
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