Interannual variations in
the atmospheric heat budget Kevin E. Trenberth, David P. Stepaniak, and Julie M. Caron JOURNAL OF GEOPHYSICAL RESEARCH, VOL.
Since then, satellite reading of temperatures and the occlusion of numerous infrared bands, ground based, aircraft and balloon measurements of same, and an ever - increasing data base of the optical properties of CO2 (and other gases, like water vapour), have helped refine radiation calculations towards determining
the atmospheric heat budget.
Not exact matches
Increasing
atmospheric CO2 concentrations cause an imbalance in Earth's
heat budget: more
heat is retained than expelled, which in turn generates global surface warming.
If we had launched the Triana / DSCOVR climate satellite ten years ago, instead of mothballing it, we'd probably have robust answers to the energy
budget question, and we could get the ocean
heat change by calculating the (total energy change)- (
atmospheric warming).
The seasonal evolution of the continental
heat budget for different monsoon systems (Fig. 2) shows that sensible
heat flux from the land surface increases during spring and
heats up the
atmospheric column prior to the rainy season.
We have to consider trends in the
heat budget of the oceans and what that portends for future
atmospheric warming.
«To better monitor Earth's energy
budget and its consequences, the ocean is most important to consider because the amount of
heat it can store is extremely large when compared to the land or
atmospheric capacity,» said Yan.
His research involves studies of the role of the tropics in mid-latitude weather and global
heat transport, the moisture
budget and its role in global change, the origins of ice ages, seasonal effects in
atmospheric transport, stratospheric waves, and the observational determination of climate sensitivity.
Black et al. (15) analyzed basic factors that likely contributed to the summer 2003 European
heat wave, examining large - scale
atmospheric flow, regional
heat budget at the top of the atmosphere, and sea surface temperature.
I know many clever scientists have produced figures calculating the
heat budget of the
atmospheric greenhouse effect but the value to be fixed to the convective process as a negative forcing has not been adequately quantified as far as I know.
Simpson began with a gray - body calculation, Simpson (1928a); very soon after he reported that this paper was worthless, for the spectral variation must be taken into account, Simpson (1928b); 2 - dimensional model (mapping ten degree squares of latitude and longitude): Simpson (1929a); a pioneer in pointing to latitudinal transport of
heat by
atmospheric eddies was Defant (1921); for other early energy
budget climate models taking latitude into account, not covered here, see Kutzbach (1996), pp. 354 - 59.
Fasullo and Trenberth (2008b) went on to evaluate the temporal and spatial characteristics of meridional
atmospheric energy transports for ocean, land, and global domains, while Trenberth and Fasullo (2008) delved into the ocean
heat budget in considerable detail and provided an observationally based estimate of the mean and annual cycle of ocean energy divergence and a comprehensive assessment of uncertainty.