Those clouds will find more intense
microphysics changes near the negative aspect of the capacitive coupling — namely on the ocean surface, given that the ionosphere is positively charged by thunderstorms globally.
Here is an example of a changing entropy pattern, just like the increase in hurricane intensity, brought about by
microphysics changes which have occurred due directly to increases of CO2 changing the CONDUCTIVITY of oceans.
Not exact matches
This new study then looked at how
changes in
microphysics of the air - sea interface can make a storm grow or weaken in intensity.
Scientists have some idea of how aerosols
change a cloud's inner workings but the
microphysics of charge separation and lightning generation are still not fully understood.
The conductivity
changes impact cloud
microphysics, and heat trapped or released out into space.
He based his main skeptical ideas on the SOI index — which is ironically causally about CO2 coming out of solution in the Pacific, to one side or the other, and impacting surface conductivities associated with the capacitive couplings I am writing about that
change cloud
microphysics.
The most significant
changes in the new D - series cloud datasets are: 1) revised radiance calibrations to remove spurious
changes in the long - term record, 2) increased cirrus detection sensitivity over land, 3) increased low - level cloud detection sensitivity in polar regions, 4) reduced biases in cirrus cloud properties using an ice crystal
microphysics model in place of a liquid droplet
microphysics model, and 5) increased detail about the variations of cloud properties.
On the basis of the current density - cloud hypothesis the variations in the current density
change the charge status of aerosols that affect the ice production rate and hence the cloud
microphysics and climate [e.g., Tinsley and Dean, 1991; Tinsley, 2000].
Additionally, climatological models, which incorporate CCN generation mechanisms and cloud
microphysics, fail to produce significant
change in global - scale CCN populations, cloud optical properties, or radiative forcing (Snow - Kropla et al. 2011; Dunne et al. 2012; Kazil et al. 2012).
Using a full factorial design, three schemes were
changed in the MPE: vertical diffusion, cloud
microphysics, and cumulus convection.