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Fig. 12. Illustration chart about the general approach and connections between observations and modeling efforts which should lead to the development of state-of-the-art thermosphere-exosphere models and to a better understanding of aeronomically related atmospheric evolution aspects for terrestrial planets.
The chapter focuses on the relation between observations and modeling results.
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Overall, the results do not suggest immediate concern for current water resource management on the basis of observed trends alone; however, the differences between observations and model projections suggest these findings should not be viewed complacently, and greater reconciliation between data- and model-based assessments should be sought as a basis for informing water management decisions.
They state, "There is no significant discrepancy between observations and models for lapse rate change between the surface and the full troposphere".
Aerosol Comparisons between Observations and Models.
The agreement between observations and models is still only qualitative for many parameters.
In addition, the SPRINTARS model is included in the Aerosol Comparisons between Observations and Models (AEROCOM) project (e.g., Kinne et al. 2006).
The observed magnetopause locations are compared with an empirical magnetopause model of Shue et al. (1997) and the sources of differences between observations and model predictions are analyzed.
Transformation of annual extreme values to SPI and subsequent interpolation to coarser grids are carried out to facilitate comparison between observations and model simulations.
The concept of the coronal heating is therefore proven, while many details still have to be improved before getting a perfect match between observations and model.
IRT also enables to asses specific discrepancies between observations and model predictions, known as residuals, to evaluate whether the intended inferences made from the model are trustworthy (Glas, 2016).
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