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Technical Report No. ? - DKRZ

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<strong>DKRZ</strong> GRIB/EXTRA Format Module Documentation<br />

IV. For description of soil temperatures see section 3.7.2<br />

V. The planetary albedo (code 380 and 381, respectively for clear sky) equals zero, if the numerator is zero.<br />

Calculate albedos only from temporal or eventually spatial mean fluxes. The global mean results<br />

from the glogal mean of fluxes !<br />

<strong>No</strong>te: For a description of method I and method II of calculating clear sky diagnostics and cloud forcing<br />

refer to <strong>DKRZ</strong> <strong>Technical</strong> <strong>Report</strong> <strong>No</strong>. 6, The ECHAM3 Atmosphere Model, Appendix F.<br />

T s<br />

T Sn<br />

T D3<br />

T D4<br />

T D5<br />

T D<br />

T DCL<br />

surface temperature (interface to the atmosphere)<br />

snow temperature<br />

soil temperatures<br />

Figure 1 Description of soil temperatures in the ECHAM model. 1<br />

For detailed description of soil processes refer to <strong>DKRZ</strong> <strong>Technical</strong> <strong>Report</strong> <strong>No</strong>. 6, The<br />

ECHAM3 Atmosphere Model, section 3.13 .<br />

1. <strong>No</strong>te that the surface temperature T s is always the interface temperature to the atmosphere even in<br />

snow coverded areas.<br />

PAGE 3.3.7

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