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High frequency wind-related seasonal mean latent heat flux changes
Climate Dynamics, 2020Surface 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
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The surface latent heat flux anomalies related to major earthquake
SPIE Proceedings, 2011SLHF (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
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An attenuated eddy covariance method for latent heat flux measurements
Water Resources Research, 2007An 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
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Sensitivity of C2 sub n to Random Variations of Windspeed, Sensible Heat Flux, and Latent Heat Flux
1992Abstract : 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
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Estimation of bulk transfer coefficient for latent heat flux (Ce)
Boundary-Layer Meteorology, 1991The 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.
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Review and assessment of latent and sensible heat flux accuracy over the global oceans
Remote Sensing of Environment, 2017Keith Haines, Maria Valdivieso
exaly

