A methodology to define uncertainties associated with ocean surface heat flux calculations has been developed and applied to a revised version of the Oberhuber global climatology, which utilizes a summary of the COADS surface observations. Systematic and random uncertainties in the net oceanic heat flux and each of its four components at individual grid points and for zonal averages have been estimated for each calendar month and the annual mean. The most important uncertainties of the 2{degree} x 2{degree} grid cell values of each of the heat fluxes are described. Annual mean net shortwave flux random uncertainties associated with errors in estimating cloud cover in the tropics yield total uncertainties which are greater than 25 W m{sup {m...
The four components of the long-term annual mean net surface heating of the tropical Pacific Ocean b...
International audienceOcean-atmosphere interactions represent a key component of the hydrological cy...
Ocean warming accounts for the majority of the earth's recent energy imbalance. Historic ocean heat ...
For over a decade, several research groups have been developing air-sea heat flux information over t...
Lower-bounds on uncertainties in oceanic data and a model are calculated for the 20-year time means ...
Latent heat flux (LHF) is one of the main contributors to the global energy budget. As the density ...
Four state-of-the-art satellite-based estimates of ocean surface latent heat fluxes (LHFs) extending...
Results from an analysis of the Southampton Oceanography Centre (SOC) global air–sea heat flux clima...
The exchange, or flux, of heat between the oceans and atmosphere is an important driver of the globa...
The ocean plays an important role in the climate system on timescales of weeks to centuries. Despite...
Turbulent and radiative exchanges of heat between the ocean and atmosphere (hereafter heat fluxes), ...
A dataset including daily- and monthly-mean turbulent fluxes (momentum, latent heat, and sensible he...
The surface heat flux feedback is estimated in the Atlantic and the extra-tropical Indo-Pacific, usi...
We present the first analysis of global and hemispheric surface warming trends that attempts to quan...
Estimates of the components of the surface heat flux in the Western Equatorial Pacific Ocean are pre...
The four components of the long-term annual mean net surface heating of the tropical Pacific Ocean b...
International audienceOcean-atmosphere interactions represent a key component of the hydrological cy...
Ocean warming accounts for the majority of the earth's recent energy imbalance. Historic ocean heat ...
For over a decade, several research groups have been developing air-sea heat flux information over t...
Lower-bounds on uncertainties in oceanic data and a model are calculated for the 20-year time means ...
Latent heat flux (LHF) is one of the main contributors to the global energy budget. As the density ...
Four state-of-the-art satellite-based estimates of ocean surface latent heat fluxes (LHFs) extending...
Results from an analysis of the Southampton Oceanography Centre (SOC) global air–sea heat flux clima...
The exchange, or flux, of heat between the oceans and atmosphere is an important driver of the globa...
The ocean plays an important role in the climate system on timescales of weeks to centuries. Despite...
Turbulent and radiative exchanges of heat between the ocean and atmosphere (hereafter heat fluxes), ...
A dataset including daily- and monthly-mean turbulent fluxes (momentum, latent heat, and sensible he...
The surface heat flux feedback is estimated in the Atlantic and the extra-tropical Indo-Pacific, usi...
We present the first analysis of global and hemispheric surface warming trends that attempts to quan...
Estimates of the components of the surface heat flux in the Western Equatorial Pacific Ocean are pre...
The four components of the long-term annual mean net surface heating of the tropical Pacific Ocean b...
International audienceOcean-atmosphere interactions represent a key component of the hydrological cy...
Ocean warming accounts for the majority of the earth's recent energy imbalance. Historic ocean heat ...