PP22A-03
500-year Reconstructions of Circulation in the Northeastern Pacific and Western North America: Relation to Precipitation and Fire Conditions in California and Precipitation in Hawai'i

Tuesday, 15 December 2015: 10:50
2012 (Moscone West)
Eugene R Wahl1, Eduardo Zorita2, Valerie Trouet3 and Henry F Diaz3, (1)NOAA Boulder, Boulder, CO, United States, (2)Helmholtz-Zentrum Geesthacht Centre for Materials and Coastal Research, Geesthacht, Germany, (3)University of Arizona, Tucson, AZ, United States
Abstract:
A reconstruction of the position of the North Pacific Jet Stream (NPJ) over the past 500 years is evaluated in relation to dry and wet extremes in California and extremes of Sierra Nevada fire activity. This work represents a unique combination of independent annually-resolved paleoclimate and paleoecological reconstructions in the region. Results indicate that fire and precipitation extremes are both closely linked with NPJ winter position, with characteristic wet/low fire and dry/high fire NPJ spatial features in the Pacific adjacent to western North America. These features are in turn evaluated in 21st century climate model scenarios using transient integrations over the past millennium, the instrumental period, and the 21st century. The reconstruction of NPJ position is driven by an analog process that employs independent paleoclimate field reconstructions to select model states closest to the reconstructions; it is thus logically and scientifically most consistent to use comparable models to evaluate the future in relation to the past. Initial results indicate that relatively wet/low fire regional conditions are reasonably possible in the later 21st century under a high greenhouse gas forcing regime (RCP 8.5), even though temperatures rise significantly. Related hydroclimate research reconstructs a precipitation index for the Hawai'ian Islands (HI-precip) over the past 500 years. A northeastern Pacific sea level pressure index reconstructed using the analog process is employed as the driving variable in a calibration against HI-precip. Initial reconstruction results indicate significant bicentennial spectral power, which includes a long-term drying trend that began around 1850 and continues into the first decades of the 21st century. Related statistical downscaling of climate model output for HI-precip to the end of the 21st century suggests the possibility of continued drying under RCP 8.5.