-- These storms should penetrate higher as climate warms according to the models, a positive feedback, and satellite data looking at
cloud height changes over El Nino time scales show something similar and show the models getting that about right also, for physical reasons we think we understand
Not exact matches
This new research shows the first clear evidence of the long - term effects of pollution particles on
cloud height and thickness, and how those
changes both reduce precipitation in dry regions and increase precipitation in wet regions.
This fall, NASA will launch the Ice,
Cloud, and land Elevation Satellite - 2 (ICESat - 2), which will use a highly advanced laser instrument to measure the
changing elevation of ice around the world, providing a view of the
height of Earth's ice with greater detail than previously possible.
According to thermodynamics and a largely fixed lapse rate, the average
cloud height will simply shift up and down in altitude with
change in temperature, which you can see in their Figure 2.
Regionally,
changes in relative humidity near the surface would affect the
height at which
clouds form...
Now we have a couple of mechanisms that seem realistic for several specific types of
changes such as the
cloud height feedback, and we have some observational confirmation of a general latitudinal pattern of feedbacks that many models seem to get, more so than was the case a decade ago.
Ignore the movements of
clouds; wind direction normally
changes with
height.
More surface warming than
cloud -
height warming is indicative of surface albedo
change and / or fewer
clouds and / or increase in solar «constant».
For instance, researchers still don't completely understand the role of aerosols in the atmosphere, the variable effects of
clouds at different
heights, and the influence of feedback mechanisms such as the
changing reflectivity of the Earth's surface and the release of gases from permafrost or deep seabeds.
Only in this way is the energy balance determined empirically and the multitude of
changes —
cloud height and extent, water vapour, ozone, surface temperature, ice and snow, biology, aerosols — integrated in a comprehensible measure.
There can be interruptions when low
cloud causes lower T, there can be nearby vegetation that casts a shadow on the screen sometimes, other vegetation effects like when mowed surrounding grass
changes the effective
height above ground of the thermometer, there can be a burst of rain that cools the surroundings — and so on into the night.
We know these
clouds are related to low - level stability, but they also are affected by shallow convection, precipitation processes, and
changes in the capping inversion
height.
They note a reduction in the base
height of low level
clouds of approximately 7 m during dates of high GCR flux and based on periodogram analysis methods conclude that
changes in the base
height of stratiform
clouds may show the presence of the 27 - day and 1.68 - year solar periods.
Cloud top height changes are quite well described by the fixed anvil temperature hypothesis of Hartmann and Larson; cloud base heights change little, remaining near the same pres
Cloud top
height changes are quite well described by the fixed anvil temperature hypothesis of Hartmann and Larson;
cloud base heights change little, remaining near the same pres
cloud base
heights change little, remaining near the same pressure.
There has been some
changes in
cloud height in the tropics though.
The SGM doesn't have
clouds and even if you put in an absorber with a different scale
height like water vapor, it's never saturated, so there are no phase
changes above the surface.
Percent
change in zonally - averaged
cloud cover over the oceans as a function of latitude and
height in response to an instantaneous quadrupling of CO2, decomposed into two parts: (a) a fast adjustment that occurs before surface temperatures have warmed appreciably, and (b) a part that scales linearly with the warming of surface temperature as the system adjusts to the increase in CO2.
Zhanqing Li, lead author of a paper published in Nature Geoscience and University of Maryland atmospheric scientist, says, «Using a 10 - year dataset of atmospheric measurements, we have uncovered the long - term, net impact of aerosols on
cloud height and thickness and the resulting
changes in precipitation frequency and intensity.»