Popp, M., Schmidt, H. & Marotzke, J. Transition to a moist greenhouse state with CO2 and solar forcing.
For a semimajor axis of 1.140 a.u., the planet goes into a Moist Greenhouse state, whereas a semimajor axis of 1.225 a.u.
In terms of mean TSI we find a habitable climate between 0.954 and 1.004 S0 with TSI values between 0.907 and 0.954 S0 leading to a transition to a Snowball and a TSI between 1.004 and 1.052 S0 leading to a Moist Greenhouse state.
Puerto Rico's transformation from a dry savanna environment to its present moist, forested state led to mass extinctions, especially of the vertebrate fauna.
The Snowball states are in red, the habitable states in yellow and blue and the Moist Greenhouse states in black.
Moist Greenhouse states are characterized by an upper atmosphere that is sufficiently moist for the planet to lose its entire water inventory to space in its lifetime as a consequence of the photo-dissociation of water and the subsequent escape of hydrogen to space.
We found that the sensitivity of PP to soil moisture deficit enhances the trigger of convective rainfall relative to HW and OF, with enhancements of about 25%and30%0% for dry moisture states, and 5%and15%5% for moist soil moisture states, respectively.
The precipitation heat energy comes from the basic state moist static energy that is largely controlled by basic state SST (Wang 1988b; Wang and Li 1994).
Finally, we have shown the effect of temperature on thermal conductivity for both moist and dry states.
In this paper, the effects of curing conditions (dry air, moist air and water), state of water (static water and flowing water) and initial air curing time (5 h, 3 d and 28 d) on the corrosion behavior of magnesium potassium phosphate cement (MKPC) paste subjected to water attack were investigated.
