Not exact matches
The higher sensitivity of the cerebellum to what we interpret to
reflect changes in vascular reactivity with marijuana abuse is consistent with clinical findings that report strokes associated with marijuana abuse are more frequently localized
in the posterior
circulation and ischemia is most frequently observed
in cerebellum (25, 54 ⇓ — 56).
What is true is that there is very very strong evidence from paleoclimate data (deep sea sediment cores) for
changes in the distribution of chemical tracers that must
reflect changes in the deep
circulation in the Atlantic.
One would want some supporting physics
in terms of
circulation changes that are
reflected in models and obs or similar.
If the objective was to develop a general
circulation model that matches reality rather than to push an agenda likely one of model fixes would be modify to GCMs (modeling of planetary cloud cover) to match Lindzen and Choi finding that planetary cloud cover
in the tropics increases or decreases to resist forcing
changes by
reflecting more or less radiation off to space.
As sub-surface oxygen concentrations
in the ocean everywhere
reflect a balance between supply through
circulation and ventilation and consumption by respiratory processes, the absolute amount of oxygen
in a given location is therefore very sensitive to
changes in either process, more sensitive perhaps as other physical and chemical parameters.
They concluded, «ocean pH does not simply
reflect atmospheric CO2 trends but rather that
circulation / biogeochemical
changes account for > 90 % of pH variability
in the Sargasso Sea and more variability
in the last century than would be predicted from anthropogenic uptake of CO2 alone.»
Diversity differences between areas may also
reflect changes in water masses and
circulation [305], [306] as well as
changes in temperature and salinity [307].
They also suggest that there would be complex spatial patterns of response â $ «local warming
in the lower stratosphere, increases
in reflected solar radiation, decreases
in outgoing longwave radiation, dynamical
changes in the northern hemisphere winter
circulation, decreases
in tropical precipitation etc..
D / O events tended to be short term and usually hemispheric, typically
reflecting changes in ocean
circulation patterns that produced NH effects opposite those
in Antarctica.