No, Frankie boi, as explained many times, the residence time for H2O in the atmosphere is about ten days. So H2O is a feedback from the GHGs with much longer residence times, CO2 and and CH4.
While your statement is factually correct, you also have to remember that while the residence time is 10 days, the H2O in the atmosphere is being perpetually replenished.
Mark
Of course it is. And the determining factor is the temperature of the atmosphere and water. And the GHGs determine the temperature of the atmosphere and water. Without the GHGs in the atmosphere we would have ice on the oceans clear down to the equator. That has actually happened in deep geological time.
"Snowball Earth" Confirmed: Ice Covered Equator
So why bring it up? If H2O is perpetually replenished, the residence time means nothing.
Mark
Is it now? How then did the Snowball Earth situation come to be? If the atmosphere is very cold, it will not hold much water vapor. So, if there is a serious deficit of GHGs in the atmosphere, there will be little water vapor in the atmosphere. Water vapor in the atmosphere is a feedback effect of the GHGs in the atmosphere.
I don't know what happened in the past. No one does. So tell me, how did the Earth climb out of the "snowball" situation?
Mark
On the contrary, in the last 50 years we have learned much about the prior times. You are setting in front of the greatest machine that was ever invented for education, use it.
New research sheds light on end of Snowball Earth period
New research sheds light on end of Snowball Earth period
Posted on 24 Aug 2015
The second ice age during the Cryogenian period was not followed by the sudden and chaotic melting-back of the ice as previously thought, but ended with regular advances and retreats of the ice, according to research published by scientists from the University of Birmingham in the journal
Nature Geoscience today (24 August 2015).
The researchers also found that the constant advance and retreat of ice during this period was caused by the Earth wobbling on its axis.
These ice ages are explained by a theory of Snowball Earth, which says that they represent the most extreme climatic conditions the world has ever known and yet they ended quite abruptly 635 million years ago. Little was known about how they ended - until now.
For the study, the scientists analysed sedimentary rocks from Svalbard, Norway that were laid down in that ice age. The deposits preserved a chemical record which showed high levels of CO2 were present in the atmosphere. Carbon dioxide was low when the ice age started, and built up slowly over millions of years when the whole Earth was very cold - this period is represented only by frost-shattered rubble under the sediments.
Eventually the greenhouse warmth in the atmosphere from carbon dioxide caused enough melting for glaciers to erode, transport and deposit sediment. The sedimentary layers showed ice retreat and advance as well as cold arid conditions. They reveal a time when glacial advances alternated with even more arid, chilly periods when the glaciers retreated, rivers flowed, lakes formed, and yet simple life survived.
As theory predicts, this icy Earth with a hot atmosphere rich in carbon dioxide had reached a ‘Goldilocks’ zone – too warm to stay completely frozen, too cold to lose its ice, but just right to record more subtle underlying causes of ancient climate change.
The geological researchers invited a French group of physicists who produce sophisticated climate models to test their theory that the advances and retreats of ice during this period were caused by the Earth wobbling on its axis in 20,000 year periods. The rocks and the models agreed: slight wobbles of the Earth on its spin axis caused differences in the heat received at different places on the Earth’s surface. These changes were small, but enough over thousands of years to cause a change in the places where snow accumulated or melted, leading the glaciers to advance and retreat. During this time the whole Earth would have looked like the Dry Valley regions of Antarctica – a very dry landscape, with lots of bare ground, but also containing glaciers up to 3 km thick.