Westerly winds impact glacier energy balance and sublimation at August-one glacier in northern Tibetan Plateau. [PDF]
Guo S, Li Y, Chen R, Liu J, Han C.
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Daily rainfall variability controls humid heatwaves in the global tropics and subtropics. [PDF]
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Seasonal predictability of an indicator of mass coral bleaching between the Pacific ocean and the East China sea with a large ensemble climate model. [PDF]
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Physically-constrained evapotranspiration models with machine learning parameterization outperform pure machine learning: Critical role of domain knowledge. [PDF]
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Towards definitive functional forms for Monin-Obukhov similarity functions in stable and very stable surface layers. [PDF]
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Characterizing the Impacts of 2024 Total Solar Eclipse Using New York State Mesonet Data. [PDF]
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Sensible and latent heat flux estimates in Antarctica
1993The assumption has been made that the net annual contribution of water by the processes of deposition and sublimation to the Antarctic Ice Sheet is zero. The U.S. Antarctic Program started installing reliable automatic weather stations on the Antarctic Continent in 1980.
Charles R. Stearns, George A. Weidner
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Description and evaluation of a sensible heat flux detector
Boundary-Layer Meteorology, 1977An eddy-correlation method is the basis of a newly-developed sensible heat-flux detector which collects air temperature information proportional to the vertical wind speed in two electronic counters, one for upflow and one for downflow. The current model uses fast-responding sensors for vertical velocity and air temperature, but the principle should be
R. Desjardins
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Recent numerical modeling studies demonstrate that dry tropical cyclones can be stably sustained via supply of surface sensible heat flux. This raises questions of whether surface sensible heat flux (SHX) and latent heat flux (LHX) have the same effect ...
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Physical connection of sensible and ground heat flux
Journal of Hydrology, 2021Abstract Characterizing physical relationships between the sensible, latent and ground heat flux at the Earth surface is of crucial importance in studying the global energy, water, and carbon cycles. Here we demonstrate an analogy between the daily mean turbulent heat transfer in the atmospheric surface layer and conductive-advective heat transfer in
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