GSTDTAP  > 气候变化
DOI10.1029/2018GL077857
Diurnal Variation of Liquid Water Path Derived From Two Polar-Orbiting FengYun-3 MicroWave Radiation Imagers
Tang, Fei1,2,3; Zou, Xiaolei4
2018-06-28
发表期刊GEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
EISSN1944-8007
出版年2018
卷号45期号:12页码:6281-6288
文章类型Article
语种英语
国家Peoples R China; USA
英文摘要

MicroWave Radiation Imagers (MWRIs) onboard the afternoon FengYun-3B (FY-3B) and midmorning FengYun-3C (FY-3C) satellites provide global observations almost 4 times a day at any location. This study examines the diurnal cycle of the liquid water path (LWP) over the southeast Pacific Ocean using MWRI data. A double-difference calibration method is first used to evaluate the MWRI calibration bias based on Tropical Rainfall Measuring Mission Microwave Imager (TMI) measurements. LWP diurnal cycle characteristics are derived from FY-3B/C MWRI data measured in 2014. The diurnal variation of LWP from combined FY-3B/C MWRI measurements are consistent with that derived from Tropical Rainfall Measuring Mission Microwave Imager data. Maximum and minimum LWPs occurred in the early morning and afternoon, respectively. The largest diurnal amplitude (similar to 40% of the mean LWP) was located near 85 degrees W/20 degrees S. The diurnal amplitude varied from season to season. MWRI data can provide important constraints for models simulating the cloud diurnal cycle.


Plain Language Summary MicroWave Radiation Imager (MWRI) dual-polarization measurements at 10.65, 18.7, 23.8, 36.5, and 89GHz can be combined to retrieve the liquid water path (LWP) in the atmosphere over ocean surfaces. The Chinese FengYun-3B and FengYun-3C satellites provide MWRI observations during their midmorning and afternoon orbits, respectively, allowing the diurnal variations of LWP to be observed globally by such polar-orbiting satellites. The diurnal variations of LWP are important for understanding hydrometeorological processes in the atmosphere and for validating LWP numerical weather prediction models. It is shown that in 2014, FengYun-3B and FengYun-3C MWRI-derived LWP retrievals compared well with those derived from the Tropical Rainfall Measuring Mission Microwave Imager over the southeast Pacific Ocean. The intensity of the diurnal cycle varied from season to season and the largest diurnal amplitude (similar to 40% of the mean LWP) was located near 85 degrees W/20 degrees S.


领域气候变化
收录类别SCI-E
WOS记录号WOS:000438499100051
WOS关键词CLOUD ; RETRIEVAL ; CIRCULATION ; OCEANS ; SSM/I ; CYCLE
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/28277
专题气候变化
作者单位1.Chinese Acad Meteorol Sci, Beijing, Peoples R China;
2.State Key Lab Severe Weather, Beijing, Peoples R China;
3.NUIST, Joint Ctr Data Assimilat Res & Applicat, Coll Atmospher Sci, Nanjing, Jiangsu, Peoples R China;
4.Univ Maryland, ESSIC, College Pk, MD 20742 USA
推荐引用方式
GB/T 7714
Tang, Fei,Zou, Xiaolei. Diurnal Variation of Liquid Water Path Derived From Two Polar-Orbiting FengYun-3 MicroWave Radiation Imagers[J]. GEOPHYSICAL RESEARCH LETTERS,2018,45(12):6281-6288.
APA Tang, Fei,&Zou, Xiaolei.(2018).Diurnal Variation of Liquid Water Path Derived From Two Polar-Orbiting FengYun-3 MicroWave Radiation Imagers.GEOPHYSICAL RESEARCH LETTERS,45(12),6281-6288.
MLA Tang, Fei,et al."Diurnal Variation of Liquid Water Path Derived From Two Polar-Orbiting FengYun-3 MicroWave Radiation Imagers".GEOPHYSICAL RESEARCH LETTERS 45.12(2018):6281-6288.
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