It has been proposed that Earth's climate could be affected
by changes in cloudiness caused by variations in the intensity of galactic cosmic rays in the atmosphere.
Not exact matches
A multidisciplinary team led
by Pacific Northwest National Laboratory's Dr. Chuck Long found that, at least
in the continental United States,
changes in clouds and
cloudiness have a greater influence on brightening than any decrease
in aerosol amounts alone.
Given that atmospheric CO2 will likely continue to climb over the next century, a long - term increase
in flowering activity may persist
in some growth forms until checked
by nutrient limitation or
by climate
change through rising temperatures, increasing drought frequency and / or increasing
cloudiness and reduced insolation.
Your earlier # 182 was equally disconcerting where you quoted Norris and Slingo (2009) saying «At present, it is not known whether
changes in cloudiness will exacerbate, mitigate, or have little effect on the increasing global surface temperature caused
by anthropogenic greenhouse radiative forcing.»
(i) Harrison and Stephenson show (see their Figure 2; reproduced
in Figure 3
in top article) a very weak correlation between the CRF and the diffuse fraction (DF)(
cloudiness — presumably dominated
by changes in low - level
cloudiness), which breaks down when the CRF is higher than 3600 (x100) per hour.
Consequently, as they say slightly earlier
in the abstract: «At present, it is not known whether
changes in cloudiness will exacerbate, mitigate, or have little effect on the increasing global surface temperature caused
by anthropogenic greenhouse radiative forcing.»
The
changes in both satellite derived and measured surface insolation data are also
in line with
changes in global
cloudiness provided
by the International Satellite Cloud Climatology Project (ISCCP), which show an increase until the late 1980s and a decrease thereafter, on the order of 5 % from the late 1980s to 2002.
The exact mechanism
by which cosmic rays then influence the climate is not known
in detail, but current efforts, mainly
by a Danish research group, focus on
changes in Earth's
cloudiness.]
Temperature
changes induced
by sun and oceans drive air circulation
changes which drive
changes in every aspect of climate including convection, conduction, evaporation, condensation, precipitation, windiness,
cloudiness, albedo and humidity as regards both quantities and distribution.
In my opinion, the most likely explanation for short term variations in temperature is due to changes in patterns of cloudiness coupled with changes in particulates in the atmosphere both of which alter the amount of sunlight getting through to and being absorbed by the ocean
In my opinion, the most likely explanation for short term variations
in temperature is due to changes in patterns of cloudiness coupled with changes in particulates in the atmosphere both of which alter the amount of sunlight getting through to and being absorbed by the ocean
in temperature is due to
changes in patterns of cloudiness coupled with changes in particulates in the atmosphere both of which alter the amount of sunlight getting through to and being absorbed by the ocean
in patterns of
cloudiness coupled with
changes in particulates in the atmosphere both of which alter the amount of sunlight getting through to and being absorbed by the ocean
in particulates
in the atmosphere both of which alter the amount of sunlight getting through to and being absorbed by the ocean
in the atmosphere both of which alter the amount of sunlight getting through to and being absorbed
by the oceans.
In my opinion, measuring the heat content of the oceans can not necessarily be used to assess sensitivity since a slight change in the amount of cloudiness has a significant impact on the amout of solar radiation being received by the ocean
In my opinion, measuring the heat content of the oceans can not necessarily be used to assess sensitivity since a slight
change in the amount of cloudiness has a significant impact on the amout of solar radiation being received by the ocean
in the amount of
cloudiness has a significant impact on the amout of solar radiation being received
by the oceans.
This
change is explained
by a decrease
in subtropical and mid-latitude low
cloudiness, along with a reduction
in high - latitude surface albedo due to decreased sea ice.