HR: 0830h
AN: A31E-0104    [PDF]
TI: Climate Response to Large-Scale Wind Farms
AU: * Malyshev, S L
EM: malyshev@princeton.edu
AF: Princeton University, Guyot Hall, Princeton, NJ 08544 United States
AU: Pacala, S W
EM: pacala@Princeton.EDU
AF: Princeton University, Guyot Hall, Princeton, NJ 08544 United States
AU: Keith, D W
EM: keith@cmu.edu
AF: Carnegie Mellon University, 129 Baker Hall, Pittsburgh, PA 15213-3890 United States
AU: Denkenberger, D C
EM: ddenkenb@Princeton.EDU
AF: Princeton University, Guyot Hall, Princeton, NJ 08544 United States
AU: Roy, S B
EM: sroy@Princeton.EDU
AF: Princeton University, Guyot Hall, Princeton, NJ 08544 United States
AU: Shevliakova, E
EM: elena@eno.Princeton.EDU
AF: Princeton University, Guyot Hall, Princeton, NJ 08544 United States
AB: Enhanced reliance on wind energy is one of the possible ways to solve the greenhouse gas problem. However, because wind farms modify the interaction between atmosphere and surface, there is a possibility that wind energy might also change the global climate if developed on a scale large enough to make material reductions in greenhouse emissions. To investigate possible effect of large wind farm arrays on climate, we used a version of GFDL AGCM with prescribed climatological SST and ice extent. A series of 20-year integration included a range of spatial coverage and several different parameterizations for wind farms, as well as controls. Presented here are the results of the experiments with the largest wind farm arrays considered, where significant parts of Europe,North America, andChinaare covered. The total wind farm area in this case is about 10% of land surface; the resulting dissipation of kinetic energy on wind farms ranges from 12 to 19 TW (compared to current global primary energy consumption of 12 TW). The results of the simulations show similar effects on climate despite differences in parameterization for the wind farms. The global-average climate reaction is negligible, but regional effects are not. The effect of wind farms on annual mean surface air temperature reaches a regional maximum of the order of 1 degree, which is smaller than the 2XCO2 signal. The temperature response is strongest inEurasia, where it is characterized by cooling in northern mid-latitudes of entire continent and warming in the South in all seasons except JJA, when the pattern is much weaker. The response of precipitation does not show an obvious large-scale pattern and is likely to be statistically not significant.
DE: 1610 Atmosphere (0315, 0325)
DE: 1620 Climate dynamics (3309)
DE: 3307 Boundary layer processes
DE: 3322 Land/atmosphere interactions
DE: 3337 Numerical modeling and data assimilation
SC: Atmospheric Sciences [A]
MN: 2003 Fall Meeting