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Possible climatic impact of large scale solar thermal energy production. [Mathematical model]

Conference ·
OSTI ID:7310858
The ZAM2 (zonal atmospheric model) was used to estimate the climatic effects of large scale solar thermal power facilities. The results appear to be consistent with other numerical experiments. The model response can be summarized by tracing through a feedback loop: decreased surface albedo ..-->.. warmer surface ..-->.. increased evaporation and increased convection ..-->.. increased precipitation in the subtropics and increased water vapor in high latitudes ..-->.. increased surface temperatures at high latitudes ..-->.. decreased equator-to-pole temperature gradient ..-->.. decreased Hadley cell intensity ..-->.. possible northward shift of the ITCZ (intertropical convergence zone). The experiment also resulted in a warmer upper troposphere, particularly over the latitudes of maximum area of albedo change. The response was noted in Ellsaesser et al. (1976). The increased surface energy subsequently increased surface absolute humidity which in turn displaced the convective parcel ascent curve to the right (indicating more water vapor and latent heat release) making the lapse rate less steep and warmer where the water vapor content was lowest. It should be noted that ZAM2 has previously been shown to duplicate quite well the results of a 3-D GCM for large surface perturbations, which is important because it is questionable whether experiments looking at such small changes in local albedo as reported here would be possible given the synoptic variability inherent in 3-D models.
Research Organization:
California Univ., Livermore (USA). Lawrence Livermore Lab.
DOE Contract Number:
W-7405-ENG-48
OSTI ID:
7310858
Report Number(s):
UCRL-78855; CONF-761223-1
Country of Publication:
United States
Language:
English