The stratospheric correlation coefficients for Larkhill and Lerwick have a significant minimum in the winter.doi:10.1002/qj.49708235106J. K. BannonA. GilchristJohn Wiley & Sons, LtdQuarterly Journal of the Royal Meteorological SocietyBannon, J. K. and A. Gilchrist, 1956: Variation of temperature ...
The temperature in the troposphere — the lowest layer of the earth’s atmosphere — generally decreases with altitude. That’s because the troposphere’s gases absorb very little of the incoming solar radiation. Instead, the ground absorbs this radiation and then heats the tropospheric air by con...
Our analysis suggests that the trend towards increasing convective activity in the troposphere leads—at least partly—to the trend towards cooling in the tropopause region. High CAPEs are, in general, associated with high rainfall. The minimum annual temperatures were observed almost simultaneously ...
Under the different forcings, the East-Asian SAT changes are likely to be accompanied by changes in the EAWM-associated circulation. Figure 6a–c show the lower-troposphere wind changes in response to the uniform SST warming. The anticyclonic circulation anomaly is evident over the eastern and ...
The annual variation of temperature in Antarctica has interesting properties: it is largest in the stratosphere (50° to 60°C), smaller at the surface (20° to 40°C) and smallest in the troposphere (10°C). During the winter night the troposphere temperature decreases only slightly while ...
NorthernHemisphere,theopposite scenariosareobsewedincirculationanomaliesinlowerandupperpartsofthetropospherein theyearswhenthetemperaturesarehigherthannormal,ascomparedtothoseintheyears whenthetemperaturesarelowerthannormaIinthemiddleandlowerreachesoftheYangtze River(MLRYR1.Additionally,theanomalouscirculationstructurein...
Weather, as most commonly defined, occurs in thetroposphere, the lowestregionof the atmosphere that extends from theEarth’ssurface to 6–8 km (4–5 miles) at the poles and to about 17 km (11 miles) at theEquator. Weather is largely confined to the troposphere since this is where almost...
RMSEs of LST and temperature profiles in troposphere are about 1.6 K and 2 K, respectively; RMSE of WV is around 0.3 g/cm2. RMSE of LSE is less than 0.01 in the spectral interval from 10 μm to 14 μm (Wang et al. 2013). However, because ANNs perform like black boxes and can...
The annual oscillations (AO) and semi-annual oscillations (SAO) of the monthly mean zonal and meridional winds in the troposphere, stratosphere and mesosph... CR Reddi,G Ramkumar - Journal of Atmospheric and Solar-Terrestrial Physics 被引量: 44发表: 1997年 Rayleigh LIDAR and satellite (HALOE...
The annual variation of temperature in Antarctica has interesting properties: it is largest in the stratosphere (50° to 60°C), smaller at the surface (20° to 40°C) and smallest in the troposphere (10°C). During the winter night the ... H Wexler - 《Quarterly Journal of the Royal...