outgoing longwave radiation造句
例句與造句
- Over C魌e d'Ivoire, interferometrically recorded spectra of outgoing longwave radiation ).
- Radiative cooling by outgoing longwave radiation is the primary way the Earth System loses energy.
- Outgoing longwave radiation ( OLR ) has been monitored globally since 1975 by a number of successful and valuable satellite missions.
- This cooling is offset somewhat by the greenhouse effect of clouds which reduces the outgoing longwave radiation by about 31 W / m?
- Over 99 % of outgoing longwave radiation has wavelengths between 4 祄 and 100 祄, in the thermal infrared part of the electromagnetic spectrum.
- It's difficult to find outgoing longwave radiation in a sentence. 用outgoing longwave radiation造句挺難的
- Note that the last afd was a vote to Redirect to Outgoing longwave radiation . talk ) 22 : 46, 3 May 2016 ( UTC)
- The first term is equal to the change in temperature due to incoming solar radiation and outgoing longwave radiation, which changes with time throughout the day.
- At night, the absorptive effect of clouds on outgoing longwave radiation, such as heat energy from the surface, allows for warmer diurnal low temperatures in all seasons.
- In 2000, a comparison between measurements and dozens of GCM simulations of ENSO-driven tropical precipitation, water vapor, temperature, and outgoing longwave radiation found similarity between measurements and simulation of most factors.
- In the wavelength range between 4 祄 and 10 祄 the spectrum of outgoing longwave radiation overlaps that of solar radiation, and for various applications different cut-off wavelengths between the two may be chosen.
- Over the Atlas Mountains, interferometrically recorded spectra of outgoing longwave radiation show emission that has arisen from the land surface at a temperature of about 320 K and passed through the atmospheric window, and non-window emission that has arisen mainly from the troposphere at temperatures about 260 K.
- For planets with temperature-dependent sources of greenhouse gases such as liquid water and optically thin atmospheres the outgoing longwave radiation curve ( which indicates how fast energy can be radiated away by the planet ) flattens at high temperatures, reaching a horizontal asymptote the Kombayashi Ingersoll limit itself.