WebDec 29, 2015 · Surface radiative fluxes. Electromagnetic radiation received at the surface of the Earth (ocean, land, and cryosphere) in the shortwave or longwave part of the spectrum. Surface radiation balance. The sum of the incoming and outgoing shortwave and longwave radiative fluxes at the surface. Remote sensing of radiative fluxes. WebFeb 2, 2024 · 09:00:00 21:00:00. Step. (5 values) 0 3 6 9 12. Parameter. (170 values) 0 degrees C isothermal level (atm) 2 metre dewpoint temperature 2 metre temperature 10 metre U wind component 10 metre V wind component 10 metre wind gust since previous post-processing 100 metre U wind component 100 metre V wind component Boundary …
The Role of Atmospheric Rivers in Antarctic Sea Ice Variations
WebNov 1, 1997 · The heat flux uncertainty analysis is described in section 4 for each term of the surface energy balance: the net surface shortwave(SW) and longwave (LW) radiation, the latent heat flux (LH), the sensible heat flux (SH), and the net surface heat flux (N = SW + LW + LH + SH). We define all fluxes to be positive downward. Shortwave radiation (SW) is radiant energy with wavelengths in the visible (VIS), near-ultraviolet (UV), and near-infrared (NIR) spectra. There is no standard cut-off for the near-infrared range; therefore, the shortwave radiation range is also variously defined. It may be broadly defined to include all radiation with a wavelength of 0.1μm and 5.0μm or narrowly defined so as to include only radiation between 0.2μm and 3.0μm. enable ssl for apache2 ubuntu
Air-Sea Fluxes Ocean Climate Stations - NOAA Pacific …
WebAs a response, a significant difference in the surface (11%), top of the atmosphere radiative forcing (7%), and widespread atmospheric cooling are observed in the short wave domain … WebThe monthly mean shortwave (SW) radiation budget at the Earth's surface (SRB) was computed on 2.5-degree longitude-latitude resolution for the 17-year period from 1984 to 2000, using a... WebThe units are W m –2. The main energy terms are: Q s: net radiation = Earth’s IR (up) – (solar + atmospheric IR) (down) Q H: sensible heat flux (up or down) Q E: latent heat flux (up or down) Q G: surface heating (up or down) Δ Q s: surface energy storage in trees, buildings, etc. We will neglect the storage term, which is usually small ... enable ssl in edge browser