Two-dimension model of the troposphere and stratosphere has been used for an estimation of ozone and temperature changes due to anthropogenic pollution of the atmosphere. It is shown that total ozone changes in December of 2050 at 45掳N caused by anthropogenic discharges of CH 4 , N 2 O, ...
This study shed light on the long term air temperature changes in the troposphere over the Mediterranean. For this purpose, we utilized the radiosonde datasets for the barometric levels at 850, 700, 500, 300, 200, 150, and 100 hPa from seventeen meteorological stations within the Mediterranean,...
Detection of changes in the global troposphere temperature field induced by greenhouse gasesdoi:10.1029/JD091iD06p06659Several approaches to detecting the existence of a theoretically predicted CO2-induced signal in the global temperature field are investigated. It appears that a relatively thin network ...
A detailed knowledge about temperature changes in the UTLS, including structural changes and changes in the coupling between troposphere and stratosphere, is fundamental for a better understanding of atmospheric dynamics and its impacts on global and regional climate. The results indicate substantial chang...
Impacts of tropical temperature changes in the upper troposphere (UT) and the tropical tropopause layer (TTL) on tropical cyclone (TC) activity are explored. UT and lower TTL cooling both lead to an overall increase in potential intensity (PI), while temperatures 70hPa and higher have negligibl...
Temperature and ozone changes in the upper troposphere and lower stratosphere (UTLS) are important components and sensitive indicators of climate change. In this paper, variability and trends of temperature and ozone in the UTLS were investigated for the period 2002-2017 using the hi...
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...
Seasonal Changes in a Vertical Thermal Structure Producing Stable Lower-Troposphere Layers over the Inland Region of the Indochina Peninsula The authors performed a thermal budget analysis to understand the nature of seasonal changes in stable lower-troposphere layers over the inland region of t... ...
It is shown that over the TP, the trends of air temperature changes in the upper troposphere to lower stratosphere were out of phase with those in the lower to middle troposphere. Air temperature decreased and a decreasing trend appeared in the upper troposphere to lower stratosphere. The ...
Sharp and rapid changes in the sea surface temperature (SST) associated with fronts and the diurnal cycle can drive changes in the atmospheric boundary-layer stability and circulation. Here we show how a one-dimensional surface ocean model forced with either high-resolution or daily averaged surface...