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The influence of the difference in climatology can be estimated by comparing the results obtained by DDS driven by reanalysis data and Pseudo-Clim-DS.
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There are notable differences in climatology among the study regions, most importantly the inverse seasonal relationship of southeast Asian and Australian monsoons.
As a typical example, let us assume the following case: each difference in the climatology and perturbation between the two states in the spurious manifold has opposite influences on the regional climate from each other, but not in nature's manifold.
This was an indication that the difference in the climatology between the dry and rainy season as well as the land surface characteristics and the morphology of the vegetation influenced the NEE and its composite fluxes.
The first represents the difference due to the change in climatology, and this is the quantity estimated with Pseudo-Clim-DS.
The difference in precipitation resulting from climatology (Fig. 3d) is much smaller than the total difference.
Also, we compare WACCM and SC-WACCM to CCSM4, the "low-top" version of CESM1, and we find very significant differences in the stratospheric climatology and variability.
The second represents the difference due to the difference in a given perturbation under the same climatology, e.g., the influence of the number of cyclones passing through the calculation domain.
The money's in climatology!
But things are rarely so straightforward in climatology.
My parents are both professors, one in biology and the other in climatology.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com