Evaluating the lower-tropospheric COSMIC GPS radio occultation sounding quality over the Arctic

被引:17
|
作者
Yu, Xiao [1 ]
Xie, Feiqin [1 ]
Ao, Chi O. [2 ]
机构
[1] Texas A&M Univ Corpus Christi, Dept Phys & Environm Sci, Corpus Christi, TX 78412 USA
[2] CALTECH, Jet Prop Lab, 4800 Oak Grove Dr, Pasadena, CA 91109 USA
关键词
ATMOSPHERIC BOUNDARY-LAYER; TEMPERATURE; INVERSION; ASSIMILATION; PROFILES; CLOUD; UNCERTAINTIES; RETRIEVALS; SIGNALS; IMPACT;
D O I
10.5194/amt-11-2051-2018
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Lower-tropospheric moisture and temperature measurements are crucial for understanding weather prediction and climate change. Global Positioning System radio occultation (GPS RO) has been demonstrated as a high-quality observation technique with high vertical resolution and subkelvin temperature precision from the upper troposphere to the stratosphere. In the tropical lower troposphere, particularly the lowest 2 km, the quality of RO retrievals is known to be degraded and is a topic of active research. However, it is not clear whether similar problems exist at high latitudes, particularly over the Arctic, which is characterized by smooth ocean surface and often negligible moisture in the atmosphere. In this study, 3-year (2008-2010) GPS RO soundings from COSMIC (Constellation Observing System for Meteorology, Ionosphere, and Climate) over the Arctic (65-90 degrees N) show uniform spatial sampling with average penetration depth within 300m above the ocean surface. Over 70% of RO soundings penetrate deep into the lowest 300m of the troposphere in all non-summer seasons. However, the fraction of such deeply penetrating profiles reduces to only about 50-60% in summer, when near-surface moisture and its variation increase. Both structural and parametric uncertainties of GPS RO soundings were also analyzed. The structural uncertainty (due to different data processing approaches) is estimated to be within similar to 0.07% in refractivity, similar to 0.72K in temperature, and similar to 0.05 g kg(-1) in specific humidity below 10 km, which is derived by comparing RO retrievals from two independent data processing centers. The parametric uncertainty (internal uncertainty of RO sounding) is quantified by comparing GPS RO with near-coincident radiosonde and European Centre for Medium-Range Weather Forecasts ECMWF) ERA-Interim profiles. A systematic negative bias up to similar to 1% in refractivity below 2 km is only seen in the summer, which confirms the moisture impact on GPS RO quality.
引用
收藏
页码:2051 / 2066
页数:16
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