Assessing climate forcings of the Earth system for the past millennium

Physics – Geophysics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

43

Global Change: Climate Dynamics (3309), Global Change: Solar Variability, Hydrology: Anthropogenic Effects, Mathematical Geophysics: Modeling

Scientific paper

The effects of natural and anthropogenic forcings (solar activity, volcanism, atmospheric CO2 concentration, deforestation) on climate changes are estimated with the Earth system model of intermediate complexity, CLIMBER-2, for the past millennium. Simulated surface air temperatures for the Northern Hemisphere from the combined forcing correlate reasonably well with paleoclimatic data (r = 0.70). The largest negative anomalies occur when insolation minima coincide with volcanic eruptions. Anthropogenic forcings impose additional climate changes after 1850. The increasing warming from increasing CO2 concentrations is attenuated by the cooling effect from deforestation. Results from differently combined forcings suggest that the relatively cool climate in the second half of 19th century is largely attributable to cooling from deforestation.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Assessing climate forcings of the Earth system for the past millennium does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Assessing climate forcings of the Earth system for the past millennium, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Assessing climate forcings of the Earth system for the past millennium will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-997874

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.