Similarly, changes in terrestrial vegetation, such as the replacement of forests by tundra, feed back into the atmosphere
via changes in both albedo and latent heat flux from evapotranspiration.
Not exact matches
Isostatic rebound
in response to glacier retreat (unloading), increase
in local salinity (i.e., δ18Osw), have been attributed to increased volcanic activity at the onset of Bølling — Allerød, are associated with the interval of intense volcanic activity, hinting at a interaction between climate and volcanism - enhanced short - term melting of glaciers, possibly
via albedo changes from particle fallout on glacier surfaces.
For example, Fasullo and Trenberth (2012) used satellite data from the NASA Atmospheric Infrared Sounder (AIRS) and Clouds and the Earth's Radiant Energy System (CERES) to examine the relationship between seasonal
changes in relative humidity (RH)
in the dry subtropics and the Earth's
albedo via cloud cover.
Really the big question for me, once aware of all
in http://s24.postimg.org/rbbws9o85/overview.gif and much else, is whether or not coming cooling
in the 21st century will end with a somewhat brief LIA - like event, or,
via amplification of cooling through further
albedo change from snow cover rise then, continue far longer into a non-little Ice Age afterwards..
The remaining slow drift to lower GMT and pCO2 over glacial time, punctuated by higher - frequency variability and the dust − climate feedbacks, may reflect the consequences of the growth of continental ice sheets
via albedo increases (also from vegetation
changes) and increased CO2 dissolution
in the ocean from cooling.