Not exact matches
So if you think of going
in [a] warming direction of 2 degrees C compared to a
cooling direction of 5 degrees C, one can say that we might be
changing the Earth, you know, like 40 percent of the kind of
change that went on between the Ice Age; and now are going back
in time and so a 2 - degree
change, which is about 4 degrees F on a global average, is going to be very significant
in terms of
change in the distribution of
vegetation,
change in the kind of climate zones
in certain areas, wind patterns can
change, so where rainfall happens is going to shift.
Mt. MBeliling: a 1.239 meters high peak
in west Flores, offering a
cool refuge with rainforest and an ever -
changing array of
vegetation (1 hour drive from Labuan Bajo and 2 day trekking)
That is, other feedbacks come into play —
vegetation, ice sheets, aerosols, CH4 etc. will all
change as a function a warming (or
cooling), which are not included
in the standard climate sensitivity definition.
i.e.
changes in precipitation,
vegetation, deep ocean currents, etc. are at any time as likely to
cool as to heat.
The remaining slow drift to lower GMT and pCO2 over glacial time, punctuated by higher - frequency variability and the dust − climate feedbacks, may reflect the consequences of the growth of continental ice sheets via albedo increases (also from
vegetation changes) and increased CO2 dissolution
in the ocean from
cooling.
The general
cooling and atmospheric circulation
changes result
in weaker peak river flows and
vegetation productivity, which may raise issues of water availability and crop production.