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Only in the central polar basin does the annual net radiation fall below zero.
This array of instruments yielded much data, including an estimation of sea-surface temperatures, net radiation inputs to the sea surface, wave heights, and wind speeds close to the sea surface.
Net radiation.
Net radiation exchange between the two surfaces.
Net radiation fluxes dominate spring melt events.
The net radiation exchange between surfaces can be expressed as (Incropera and DeWitt 2002): left.
Rn = net radiation, G = soil heat flux, H = sensible heat and LE = latent heat.
Latent energy (LE) fluxes exceeded 70% of net radiation and 60% of potential evapotranspiration.
The net radiation and ground heat flux simulations did not change noticeable with the new RWUF.
Thus, relatively high spatial resolution net radiation data are needed for evapotranspiration studies.
STIC is driven with TS, TA, RH, net radiation (RN), and ground heat flux (G).
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