欢迎您！东篱公司
退出
-
申报数据库
-
立项数据库
-
成果数据库
-
项目获奖数据库
中文摘要：
Based on the high-resolution datasets collected in a sea fog field experiment at the northern coast of South China Sea,the variations of liquid water content (LWC) and net longwave radiation flux (NLRF) during two sea fog events on 16th-17th and 18th-19th March,2008 are exaimeed by wavelet analysis,and the cooling mechanisms for fog formation and persistence are also investigated.The main results are shown as follows.(1) Sea fog may develop and persist whether it is cloudy or not aloft.However,when there is cloud aloft the LWC is less and wind speed in sea fog is higher than that in the clear sky.(2) The quasi-periodic oscillations (QPOs) of NLRF are observed in the formation stage of the two fogs.QPOs of LWC are only found in the developing stage no matter with cloudless or cloudy condition.(3) It is likely that sea fog forms by the cooling effects of longwave radiation and develops through the vertical mixing induced by the radiative cooling at the upper level.(4) During sea fog development and persistence,other mechanisms could also play important roles in fog-layer cooling,such as turbulent heat transport and radiation transport between air-sea interfaces.
英文摘要：
Based on the high-resolution datasets collected in a sea fog field experiment at the northern coast of South China Sea,the variations of liquid water content （LWC） and net longwave radiation flux （NLRF） during two sea fog events on 16th-17th and 18th-19th March,2008 are exaimeed by wavelet analysis,and the cooling mechanisms for fog formation and persistence are also investigated.The main results are shown as follows.（1） Sea fog may develop and persist whether it is cloudy or not aloft.However,when there is cloud aloft the LWC is less and wind speed in sea fog is higher than that in the clear sky.（2） The quasi-periodic oscillations （QPOs） of NLRF are observed in the formation stage of the two fogs.QPOs of LWC are only found in the developing stage no matter with cloudless or cloudy condition.（3） It is likely that sea fog forms by the cooling effects of longwave radiation and develops through the vertical mixing induced by the radiative cooling at the upper level.（4） During sea fog development and persistence,other mechanisms could also play important roles in fog-layer cooling,such as turbulent heat transport and radiation transport between air-sea interfaces.
同期刊论文项目
同项目期刊论文
The impacts of the summer Asian Jet Stream biases on surface air temperature in mid-eastern China in
Remote influence of North Atlantic SST on the equatorial westerly wind anomalies in the western Paci
Impacts of tropical Indian Ocean SST on the meridional displacement of East Asian jet in boreal summ
Modulation of Low-latitude West Wind on Abnormal Track and Intensity of Tropical Cyclone Nargis (200
Interdecadal modulation of the influence of La Nina events on mei-yu rainfall over the Yangtze River
Effects of the East Asian summer monsoon on tropical cyclones genesis over the South China Sea on an
The impacts of the Summer Asian Jet Stream biases on surface air temperature in Middle Eastern China
The Impact of Indian Ocean variability on high temperature extremes across south of Yangtze River Va
Numerical investigation on propulsion of the counter-wind current in the northern South China Sea in
trengthening of tropical Indian Ocean teleconnection to the Northwest Pacific since the mid-1970s: A
Asymmetric modulation of the Western North Pacific cyclogenesis by the Madden-Julian Oscillation und
Decadal variability of twentieth-century El Nino and La Nina occurrence from observations and IPCC A
Evaluation of a satellite-derived latent heat flux product in the South China Sea: A comparison with
Dynamics of eddy-driven North Atlantic Oscillations in a latitudinally fluctuating jet: isolated str
位置：