Exact(60)
All points lie between the horizontal lines representing measured acf statistically indistinguishable from zero. Figure 4 Insolation year (k) vs. Insolation year (k+1) from 1975 to 2004.
Paleoclimate sensitivity to CO2 and insolation.
The increased insolation, reduced humidity, and desiccating winds contribute greatly to water loss in the lake.
Plants utilize CO2, water, and solar insolation to convert CO2 to diatomic oxygen (O2).
The temperature and salinity of its waters vary with seasonal variations in upwelling, insolation, and flow.
Those three parameters govern the amount of solar radiation (insolation) that strikes Earth's surface at different latitudes in different seasons.
A key difference is that CO2 was not as high as today, but insolation forcing was much higher.
This persistent circulation mechanism transports heat from the latitudes of greatest solar insolation to the latitudes of the subtropical ridges.
These breezes are strongest in warm, clear, dry weather, when daytime insolation, or solar radiation, is most intense.
Global horizontal insolation.
We no longer assume constant insolation.
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