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Nicholas A. Bond
Meghan F. Cronin
, and
Matthew Garvert

for the control experiment is from the Advanced Microwave Scanning Radiometer for Earth Observing System (AMSR-E) dataset valid at 13 October 2004 ( Fig. 1 ). The warm and cool perturbation SST experiments use the control SST distribution and impose SST anomalies with maximum perturbations of 1.5°C at 35°N, 140°W, tapering off to background values in a Gaussian manner with e -folding scales of 8° in latitude and 16° in longitude ( Fig. 2 ). The shape and magnitude of these SST perturbations

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