Observed Global Climate
DOI: 10.1007/10730550_26
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10 Energy budget at the earth's surface (Part 2/2)

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Cited by 4 publications
(6 citation statements)
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“…Information from direct observations at the surface as provided by GEBA is therefore particularly valuable to constrain these fluxes. A first estimation of the geographical distribution of the individual surface energy balance components based on direct observations from GEBA was performed by Ohmura and Gilgen (1993) and updated in Ohmura and Raschke (2005). Wild et al (1998b) used a combination of GEBA data and respective biases of a climate model to infer the magnitudes of the global mean energy balance components.…”
Section: Estimation Of the Global Energy Balancementioning
confidence: 99%
“…Information from direct observations at the surface as provided by GEBA is therefore particularly valuable to constrain these fluxes. A first estimation of the geographical distribution of the individual surface energy balance components based on direct observations from GEBA was performed by Ohmura and Gilgen (1993) and updated in Ohmura and Raschke (2005). Wild et al (1998b) used a combination of GEBA data and respective biases of a climate model to infer the magnitudes of the global mean energy balance components.…”
Section: Estimation Of the Global Energy Balancementioning
confidence: 99%
“…Several years later during the Atmospheric Model Intercomparison Project (AMIP II for IPCC AR4) it became possible to compare annual mean global solar irradiance at the surface from 20 participating GCMs against 760 sites for which GEBA possessed data of good quality ). The mean performance of the GCMs was an overestimation by 9 W m -2 , with a range from underestimation by 9 W m -2 (MRI) to overestimation by 31 W m -2 (COLA) (Wild, 2005 (Ohmura and Raschke 2005;Wild et al 2013). The models still overestimate solar irradiance at the surface, although the degree of the overestimation has been considerably reduced over the last 20 years.…”
Section: -1964mentioning
confidence: 96%
“…The present section is dedicated to the annual mean surface fluxes produced in the control run of ECHAM4/T106 experiments that came closest to the observed fluxes stored in GEBA. For those interested in more detailed information, such as the seasonal fluxes, it is recommended to refer to Ohmura and Raschke (2005). Figure 4a illustrates the distribution of annual global radiation, which resembles very closely Budyko (1980).…”
Section: Energy Exchange On the Earth's Surfacementioning
confidence: 99%
“…Below briefly describes the five-layer slab thermal diffusion scheme based on [1], [33]- [35]. The surface energy balance is usually defined with respect to an active layer of infinitesimal small thickness.…”
Section: Lsms and Five-layer Thermal Diffusion Schemementioning
confidence: 99%
“…The surface energy balance is usually defined with respect to an active layer of infinitesimal small thickness. In this case, the storage of energy in the layer can be neglected and the energy balance equation takes the form [33], [34] …”
Section: Lsms and Five-layer Thermal Diffusion Schemementioning
confidence: 99%