[1] This paper analyzes and attributes spatial and temporal patterns of changes in the diurnal cycle of land surface air temperature in 20 simulations from 11 global coupled atmosphere-ocean general circulation models during the 20th century and the 21st century under the SRES A1B scenario. Most of the warming in the maximum (Tmax) and minimum (Tmin) temperatures from 1900 to 2099 is attributed...

This paper evaluates sea surface temperature (SST) biases of coupled models participating in Coupled Model Intercomparison Project Phase 5 (CMIP5) and CMIP6. Overall, CMIP6 perform better than CMIP5 ones reproducing SST climatology, with lower multi-model ensemble mean (MME) globally averaged absolute bias (1.17 vs. 1.31 K). MME global annual shifts from cooling (−0.09 ± 0.52 K) to warming (0.2...

The paper "ENSO surface shortwave radiation forcing over the tropical Pacific" by Pavlakis et al adds the shortwave component to their earlier study, published in this journal, which examined ENSO surface longwave radiation forcing. The paper is fine, but the results basically corroborate previously published work regarding the evolution of ENSO induced changes in atmospheric circulation, outgo...

[1] Clear sky downwelling longwave radiation (Rldc) and cloudy sky downwelling longwave radiation (Rld) formulas were tested across eleven sites in Florida. The Brunt equation, using air vapor pressure and temperature measurements, provides the best Rldc estimates with a root mean square error of less than around 12 Wm 2 across all sites. The Crawford and Duchon’s cloudiness factor with Brunt e...

This paper addresses the refinement and testing of a simple downwelling longwave radiation model. Oklahoma atmospheric surface-layer instrumentation system (OASIS) radiation data in combination with Oklahoma Mesonet weather data were used to evaluate various techniques for estimating downwelling longwave radiation, for daytime and nighttime as well as clear and cloudy skies. The Brutsaert [Wate...

Introduction Closing the surface energy budget (SEB) is one of the longest outstanding problems in micro-meteorology. At the earth’s surface the net radiation (QN), consisting of the budget of shortwave incoming (K), shortwave outgoing (K), longwave incoming (L) and longwave outgoing radiation (L), should be balanced by the transport of heat into the soil (G) and to the atmosphere in the form o...

Radiative fluxes in the ECHAM5 general circulation model (GCM) are evaluated using both surface and satellite based observations. The fluxes at the top of the atmosphere (TOA) are generally in good agreement with the satellite data. Larger deviations in simulated cloud forcing are found especially at lower latitudes where the shortwave component within the intertropical convergence zone is over...