'Net surface heat flux' presentation slideshows

Why should we look to the ocean for low-frequency (> 1 season) variability?

Ocean Processes and Pacific Decadal Climate Variability Michael Alexander Earth System Research Lab Physical Science Division NOAA. Why should we look to the ocean for low-frequency (> 1 season) variability?. Thermal Inertia 4 m of ocean holds as much heat as atmosphere above

753 views • 56 slides

Atmospheric and Ocean Models and Their Coupling

Atmospheric and Ocean Models and Their Coupling. Xiouhua Fu International Pacific Research Center (IPRC) University of Hawaii. OUTLINE. ? Atmospheric GCM ? Intermediate Ocean Model ? Atmosphere-Ocean Coupling.

376 views • 28 slides

Heat Flux Intercomparison

458 views • 25 slides

Subtropical Mode Water: the result of air-sea interaction?

Sources and Predictability of Anomalies in North Atlantic Subtropical Mode Water Formation Using the Walin Framework ( A CLIMODE contribution) Kathryn A. Kelly University of Washington Western Boundary Current Air-sea Interaction Working Group Workshop January 2009.

425 views • 25 slides

TOGA Pan-Pacific Surface Current Study

TOGA Pan-Pacific Surface Current Study. NOAA Atlantic Oceanographic and Meteorological Laboratory (AOML) 25-26 April 1988 Miami, Florida. Background: WOCE and TOGA.

376 views • 23 slides

OEAS 604: Introduction to Physical Oceanography

442 views • 19 slides

Results from the LOCO mooring: 2003-present

262 views • 16 slides

D evelopment of a Regional Coupled Ocean-Atmosphere Model

2.2. D evelopment of a Regional Coupled Ocean-Atmosphere Model. Hyodae Seo, Arthur J. Miller, John O. Roads, and Masao Kanamitsu Scripps Institution of Oceanography. 6th Conference on Coastal Atmospheric and Oceanic Prediction and Processes

298 views • 12 slides

Fluxes at the Air-Sea Interface-- Plenary

Fluxes at the Air-Sea Interface-- Plenary. AGCMs (Bretherton) and NWPs (Jiang) exhibit moderate disagreement in surface flux components over the tropical E Pacific. NWP flux improvement when use COARE with NWP state var.

125 views • 2 slides

Ocean feedbacks on the Afro-Asian monsoon during the Mid-Holocene

Local feedback. SLP decrease. SST. Wind-Evap-SST Feedback (over 10-20N). Trade Wind (E) over ocean 10-20N. Summer Insolation. Land-sea contrast. Monsoon Wind (W). Ekman transport From N to S (over 0-10N). More Precipitation Over West Africa. SST anomaly dipole

168 views • 1 slides