Dynamically Downscaled Climate Simulations
Simulated global changes in summer (JJA) air
temperature over the past 21,000 yr. The 3,000-yr
time series shows how summer temperatures of
the past differed from the pre-industrial period (PI).
The temperature differences reflect the influence
of continental ice sheets (darkest blue), changing
atmospheric trace gases and changes in Earth-Sun
geometry (reddest colors).
temperature over the past 21,000 yr. The 3,000-yr
time series shows how summer temperatures of
the past differed from the pre-industrial period (PI).
The temperature differences reflect the influence
of continental ice sheets (darkest blue), changing
atmospheric trace gases and changes in Earth-Sun
geometry (reddest colors).
Why is this research important?
Understanding how hydrologic and ecological systems respond to and interact with climate is a pressing need in the context of future climate change. We are testing climate model simulations with geologic data to evaluate the ability of models to reproduce known past changes and to build confidence in their projections of the future. There is a well-established need for climate information at spatial and temporal resolutions that are relevant to processes on the landscape. We are addressing that need, for both paleo and future climate-based research, by producing long (i.e., multi-decadal to multi-century) simulations of past, present and future with regional climate models.
Principal Investigator: Steve Hostetler, National Research Program, Western Region in Menlo Park, CA
Project Team: Jay Alder, Andrea Allan

