Trends and solar cycle effects in temperature versus altitude from the Halogen Occultation Experiment for the mesosphere and upper stratosphere

Author:

Remsberg Ellis E.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference31 articles.

1. Cooling of the mesosphere and lower thermosphere due to doubling of CO2;Akmaev;Ann. Geophys.,1998

2. A model estimate of cooling in the mesosphere and lower thermosphere due to the CO2 increase over the last 3–4 decades;Akmaev;Geophys. Res. Lett.,2000

3. Impact of middle-atmospheric composition changes on greenhouse cooling in the upper atmosphere;Akmaev;J. Atmos. Sol. Terr. Phys.,2006

4. Coupled chemistry climate model simulations of the solar cycle in ozone and temperature;Austin;J. Geophys. Res.,2008

5. A fourteen year monthly climatology and trend in the 35–65 km altitude range from Rayleigh Lidar temperature measurements at a low latitude station;Batista;J. Atmos. Sol. Terr. Phys.

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