Abstract
The observed diurnal temperature range (DTR) displays remarkable change during last 30 years. Land air DTR generally decreases under global climate warming due to more significant night minimum temperature increase in comparison with day maximum temperature increase. Atmosphere hydrological cycle characteristics change under global warming and possible background aerosol atmosphere content change may cause essential errors in the estimation of DTR tendencies of change under global warming. The result of this study is the investigation of cloudiness effect on the DTR and blackbody radiative emissivity diurnal range. It is shown that in some cases (particularly in cold seasons) it results in opposite change in DTR and BD at doubled CO{sub 2} atmosphere content. The influence of background aerosol is the same as the cloudiness one
Eliseev, A V;
Bezmenov, K V;
Demchenko, P F;
Mokhov, I I;
Petoukhov, V K
[1]
- Russian Academy of Sciences, Moscow (Russian Federation). Inst. of Atmospheric Physics
Citation Formats
Eliseev, A V, Bezmenov, K V, Demchenko, P F, Mokhov, I I, and Petoukhov, V K.
Modelling of diurnal cycle under climate change.
Finland: N. p.,
1995.
Web.
Eliseev, A V, Bezmenov, K V, Demchenko, P F, Mokhov, I I, & Petoukhov, V K.
Modelling of diurnal cycle under climate change.
Finland.
Eliseev, A V, Bezmenov, K V, Demchenko, P F, Mokhov, I I, and Petoukhov, V K.
1995.
"Modelling of diurnal cycle under climate change."
Finland.
@misc{etde_428559,
title = {Modelling of diurnal cycle under climate change}
author = {Eliseev, A V, Bezmenov, K V, Demchenko, P F, Mokhov, I I, and Petoukhov, V K}
abstractNote = {The observed diurnal temperature range (DTR) displays remarkable change during last 30 years. Land air DTR generally decreases under global climate warming due to more significant night minimum temperature increase in comparison with day maximum temperature increase. Atmosphere hydrological cycle characteristics change under global warming and possible background aerosol atmosphere content change may cause essential errors in the estimation of DTR tendencies of change under global warming. The result of this study is the investigation of cloudiness effect on the DTR and blackbody radiative emissivity diurnal range. It is shown that in some cases (particularly in cold seasons) it results in opposite change in DTR and BD at doubled CO{sub 2} atmosphere content. The influence of background aerosol is the same as the cloudiness one}
place = {Finland}
year = {1995}
month = {Dec}
}
title = {Modelling of diurnal cycle under climate change}
author = {Eliseev, A V, Bezmenov, K V, Demchenko, P F, Mokhov, I I, and Petoukhov, V K}
abstractNote = {The observed diurnal temperature range (DTR) displays remarkable change during last 30 years. Land air DTR generally decreases under global climate warming due to more significant night minimum temperature increase in comparison with day maximum temperature increase. Atmosphere hydrological cycle characteristics change under global warming and possible background aerosol atmosphere content change may cause essential errors in the estimation of DTR tendencies of change under global warming. The result of this study is the investigation of cloudiness effect on the DTR and blackbody radiative emissivity diurnal range. It is shown that in some cases (particularly in cold seasons) it results in opposite change in DTR and BD at doubled CO{sub 2} atmosphere content. The influence of background aerosol is the same as the cloudiness one}
place = {Finland}
year = {1995}
month = {Dec}
}