Abstract
The delay of anthropogenic climate change caused by oceans and other slowly reacting climate system components forces us to numerical modeling as the basis of decisions. For three three-dimensional numerical examples, namely transient coupled ocean-atmosphere models for the additional greenhouse effect, internal ocean-atmosphere variability, and disturbance by soot particles from burning oil wells, the present-day status is described. From all anthropogenic impacts on the radiative balance, the contribution from trace gases is the most important.
Citation Formats
Grassl, H, Mikolajewicz, U, and Bakan, S.
Modelling of anthropogenic and natural climate changes.
Germany: N. p.,
1993.
Web.
doi:10.1007/BF01135906.
Grassl, H, Mikolajewicz, U, & Bakan, S.
Modelling of anthropogenic and natural climate changes.
Germany.
https://doi.org/10.1007/BF01135906
Grassl, H, Mikolajewicz, U, and Bakan, S.
1993.
"Modelling of anthropogenic and natural climate changes."
Germany.
https://doi.org/10.1007/BF01135906.
@misc{etde_5779204,
title = {Modelling of anthropogenic and natural climate changes}
author = {Grassl, H, Mikolajewicz, U, and Bakan, S}
abstractNote = {The delay of anthropogenic climate change caused by oceans and other slowly reacting climate system components forces us to numerical modeling as the basis of decisions. For three three-dimensional numerical examples, namely transient coupled ocean-atmosphere models for the additional greenhouse effect, internal ocean-atmosphere variability, and disturbance by soot particles from burning oil wells, the present-day status is described. From all anthropogenic impacts on the radiative balance, the contribution from trace gases is the most important.}
doi = {10.1007/BF01135906}
journal = []
volume = {80:6}
journal type = {AC}
place = {Germany}
year = {1993}
month = {Jun}
}
title = {Modelling of anthropogenic and natural climate changes}
author = {Grassl, H, Mikolajewicz, U, and Bakan, S}
abstractNote = {The delay of anthropogenic climate change caused by oceans and other slowly reacting climate system components forces us to numerical modeling as the basis of decisions. For three three-dimensional numerical examples, namely transient coupled ocean-atmosphere models for the additional greenhouse effect, internal ocean-atmosphere variability, and disturbance by soot particles from burning oil wells, the present-day status is described. From all anthropogenic impacts on the radiative balance, the contribution from trace gases is the most important.}
doi = {10.1007/BF01135906}
journal = []
volume = {80:6}
journal type = {AC}
place = {Germany}
year = {1993}
month = {Jun}
}