Differences

This shows you the differences between two versions of the page.

--- nestedradiation [2025/02/09 10:51] – created admin
+++ nestedradiation [2025/02/09 16:40] (current) – admin
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 the WRF domain.
-This page uses the model featured in RadiativeConvectiveEquilibrium to estimate
+This page uses the model featured in [[radiativeconvectiveequilibrium|Radiative Convective Equilibrium]] to estimate
 the change, or error, in the infrared heating rate within the WRF domain.
-^ {{:stn2x_hrhack.png}} ^
+^ {{ :stn2x_hrhack.png }} ^
 | Heating rates for radiative convective equilibrium (colors), together with the longwave heating rate (black) at the instant of CO2 reduction. All other temperatures and fluxes are held fixed at the instant of reduction, the model is not run out to a new equilibrium. (The new equilibrium would be simply the ''stn1x'' experiment).  The lower troposphere cools at a rate of 0.1 K per day, the stratosphere warms at a about 1 K per day.  The land surface will also cool (not shown), because downward longwave radiation to the surface is reduced from 414.7473 W m<sup>-2</sup> to 413.7178 W m<sup>-2</sup>, a reduction of 1.03 W m<sup>-2</sup>. Even without the effect of surface cooling, the change in CAPE after one day will be of order $g \frac{\Delta T}{T} \times 10,000 \mathrm{m} $ = 30 J/kg. |