On the Radiative and Dynamical Feedbacks over the Equatorial Pacific Cold Tongue De-Zheng Sun John Fasullo Tao Zhang Andres Roubicek J. Climate, 2003, Vol. 16, 2425-2432…

Collaborative Research: A Heat Budget Analysis of the Arctic Climate System Mark C. Serreze, Andrew Barrett, Andrew Slater CIRES/NSIDC, University of Colorado, Boulder, CO…

Slide 1 Estimating Diffusivity from the Mixed Layer Heat and Salt Balances Meghan F Cronin1, et al. 1NOAA Pacific Marine Environmental Laboratory 4 April 2013 - Station P…

Role of the Gulf Stream and Kuroshio-Oyashio Systems in Large-Scale Atmosphere-Ocean Interaction: A Review Authors: YOUNG-OH KWON, MICHAEL A. ALEXANDER,NICHOLAS A. BOND,…

Role of the Gulf Stream and Kuroshio-Oyashio Systems in Large-Scale Atmosphere-Ocean Interaction: A Review Authors: YOUNG-OH KWON, MICHAEL A. ALEXANDER,NICHOLAS A. BOND,…

Slide 1 Heat Flux Intercomparison Maria Valdivieso Department of Meteorology, University of Reading, UK ▶ Focus on surface heat fluxes ▶ Timeseries comparison at buoy…

Collaborative Research: A Heat Budget Analysis of the Arctic Climate System Mark C. Serreze, Andrew Barrett, Andrew Slater CIRES/NSIDC, University of Colorado, Boulder, CO…

SW (blue bars) and LH (green bars) components dominate. The SW feedback shows the greatest model diversity – linked to cloud uncertainties in East Pacific region (e.g.…