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High frequency wind-related seasonal mean latent heat flux changes

Climate Dynamics, 2020
Surface latent heat flux (LHF) is an important component in the heat exchange between ocean and atmosphere. Seasonal mean LHF changes are often interpreted using seasonal mean wind changes. The present study analyzes the high-frequency wind-induced seasonal mean LHF changes.
Renguang Wu, Yuqi Wang, Yang Jiao
openaire   +1 more source

The surface latent heat flux anomalies related to major earthquake

SPIE Proceedings, 2011
SLHF (Surface Latent Heat Flux) is an atmospheric parameter, which can describe the heat released by phase changes and dependent on meteorological parameters such as surface temperature, relative humidity, wind speed etc. There is a sharp difference between the ocean surface and the land surface.
Feng Jing   +4 more
openaire   +1 more source

An attenuated eddy covariance method for latent heat flux measurements

Water Resources Research, 2007
An attenuated eddy covariance (AEC) method is proposed, combining the use of a relatively robust three‐dimensional sonic anemometer and a ventilated capacitive hygrometer‐thermometer (CHT). The CHT is able to resolve a large enough frequency region of the water vapor density turbulent fluctuations to allow corrections for its limited time response in ...
Nelson L. Dias   +3 more
openaire   +1 more source

Sensitivity of C2 sub n to Random Variations of Windspeed, Sensible Heat Flux, and Latent Heat Flux

1992
Abstract : The optical turbulence structure parameter, (C sub n)sq, is a primary parameter in expressions used to characterize electromagnetic energy and image propagation through the atmosphere. Examples of these expressions include the receiver coherence diameter and the atmospheric modulation transfer function.
Arnold Tunick, Henry Rachele
openaire   +1 more source

Estimation of bulk transfer coefficient for latent heat flux (Ce)

Boundary-Layer Meteorology, 1991
The bulk transfer coefficient for latent heat flux (Ce) has been estimated over the Arabian Sea from the moisture budget during the pre-monsoon season of 1988. The computations have been made over two regions (A: 0–8 ° N; 60–68 ° E; B: 0–4 ° N; 56–60 ° E) with the upper computational boundary fixed at the 300 mb level.
openaire   +1 more source

BUBBLE ENERGY AND LATENT HEAT FLUX ESTIMATION

Heat Transfer Research, 2019
openaire   +1 more source

Review and assessment of latent and sensible heat flux accuracy over the global oceans

Remote Sensing of Environment, 2017
Keith Haines, Maria Valdivieso
exaly  

MODIS-driven estimation of terrestrial latent heat flux in China based on a modified Priestley–Taylor algorithm

Agricultural and Forest Meteorology, 2013
Yunjun Yao, Shunlin Liang, Jie Cheng
exaly  

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