Spatial and temporal variability of the evaporation duct in the Gulf of Aden

被引:26
作者
Zhang, Qi [1 ,2 ]
Yang, Kunde [1 ,2 ]
Shi, Yang [1 ,2 ]
机构
[1] Northwestern Polytech Univ, Key Lab Ocean Acoust & Sensing, Minist Ind & Informat Technol, Xian 710072, Shaanxi, Peoples R China
[2] Northwestern Polytech Univ, Sch Marine Sci & Technol, Xian 710072, Shaanxi, Peoples R China
关键词
marine atmospheric boundary layer; climatology; somali low-level jet; evaporation duct height cliff; marine radar; ATMOSPHERIC BOUNDARY-LAYER; FLUX-PROFILE RELATIONSHIPS; BULK PARAMETERIZATION; MICROWAVE LINK; ARABIAN SEA; MODEL;
D O I
10.3402/tellusa.v68.29792
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
An evaporation duct climatology is constructed for the Gulf of Aden using a 31-year high-resolution data set from the climate reanalysis product National Centers for Environmental Prediction Climate Forecast System Reanalysis. The climatology reveals spatio-temporal heterogeneity in the evaporation duct height (EDH) regulated by the strong interplay between the seasonal monsoon reversals and the related atmospheric and oceanic responses. It also reveals that the Gulf of Aden exhibits a special EDH distribution that is distinct from the adjacent Arabian Sea when the south-west monsoon dominates the gulf. Under these conditions, the EDH of the entire gulf is significantly higher than that of the adjoining Arabian Sea. A cliff-style EDH drop (referred to as the EDH cliff) forms at the mouth of the Gulf of Aden. Furthermore, the influence of the EDH cliff on marine radar was investigated using a ray-optics method. Based on the analysis, it was found that the local EDH significantly affects the radar detection ability beneath the evaporation duct for ships sailing in the Gulf of Aden.
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页数:14
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