Not exact matches
We have long - term experience in using atomic
layer deposition (ALD) to
increase the catalytic activity and long - term stability of high -
surface area materials.
These extended periods of cloudiness are usually a consequence of a weak
area of low pressure above the marine
layer which
increases its depth, making it more difficult for
surface heating to evaporate the clouds within it.
You know, for a little while there I even thought that Bob T himself (who is undoubtedly an interesting fellow) might even be sharp enough to appreciate that the coupling of
increased atmospheric CO2 and
increased seawater N nutrient levels to produce enhanced cyanobacterial productivity in near
surface layers of the oceans would also produce the weather - moderating effects listed above (particularly in the
areas where tropical storms are «brewed»).
The point is that this observation is not very relevant if the outcome comes from a combination of relevant and persistently warming data from
areas where the temperature is strongly correlated with
increase in the heat content of oceans, atmosphere and continental topmost
layers, and almost totally irrelevant data from
areas and seasons where and when exceptionally great natural variability of
surface temperatures makes these temperatures essentially irrelevant for the determination of longterm trends.
Precipitation:
increased freshwater / iceberg flux cools ocean mixed
layer,
increases sea ice
area, causing
increase of precipitation that falls before it reaches Antarctica, adding to ocean
surface freshening and reducing ice sheet growth.