[HTML][HTML] Satellite and in situ salinity: Understanding near-surface stratification and subfootprint variability
J Boutin, Y Chao, WE Asher, T Delcroix… - Bulletin of the …, 2016 - journals.ametsoc.org
Satellite and In Situ Salinity: Understanding Near-Surface Stratification and Subfootprint
Variability in: Bulletin of the American Meteorological Society Volume 97 Issue 8 (2016) …
Variability in: Bulletin of the American Meteorological Society Volume 97 Issue 8 (2016) …
Sea surface salinity observations from space with the SMOS satellite: A new means to monitor the marine branch of the water cycle
N Reul, S Fournier, J Boutin, O Hernandez… - Surveys in …, 2014 - Springer
While it is well known that the ocean is one of the most important component of the climate
system, with a heat capacity 1,100 times greater than the atmosphere, the ocean is also the …
system, with a heat capacity 1,100 times greater than the atmosphere, the ocean is also the …
Sea surface freshening inferred from SMOS and ARGO salinity: Impact of rain
J Boutin, N Martin, G Reverdin, X Yin, F Gaillard - Ocean Science, 2013 - os.copernicus.org
The sea surface salinity (SSS) measured from space by the Soil Moisture and Ocean Salinity
(SMOS) mission has recently been revisited by the European Space Agency first campaign …
(SMOS) mission has recently been revisited by the European Space Agency first campaign …
On the calculation of air‐sea fluxes of CO2 in the presence of temperature and salinity gradients
The presence of vertical temperature and salinity gradients in the upper ocean and the
occurrence of variations in temperature and salinity on time scales from hours to many years …
occurrence of variations in temperature and salinity on time scales from hours to many years …
Observation of large diurnal warming events in the near-surface layer of the western equatorial Pacific warm pool
A Soloviev, R Lukas - Deep Sea Research Part I: Oceanographic Research …, 1997 - Elsevier
Because of the relatively calm winds which prevail over the western Pacific warm pool, the
diurnal cycle of temperature in the near-surface layer of the ocean is often quite pronounced …
diurnal cycle of temperature in the near-surface layer of the ocean is often quite pronounced …
Review of understanding of Earth's hydrological cycle: Observations, theory and modelling
M Rast, J Johannessen, W Mauser - Surveys in Geophysics, 2014 - Springer
Water is our most precious and arguably most undervalued natural resource. It is essential
for life on our planet, for food production and economic development. Moreover, water plays …
for life on our planet, for food production and economic development. Moreover, water plays …
Barrier layer formation during westerly wind bursts
MF Cronin, MJ McPhaden - Journal of Geophysical Research …, 2002 - Wiley Online Library
Barrier layers between the base of a shallow halocline and the top of the thermocline are a
common feature of the western Pacific warm pool. In this paper, we investigate barrier layer …
common feature of the western Pacific warm pool. In this paper, we investigate barrier layer …
Coupled Ocean‐atmosphere response experiment (COARE): an interim report
JS Godfrey, RA Houze Jr, RH Johnson… - Journal of …, 1998 - Wiley Online Library
This paper is an interim report on results of the Coupled Ocean‐Atmosphere Response
Experiment (COARE), conducted from November, 1992, through February, 1993, in the …
Experiment (COARE), conducted from November, 1992, through February, 1993, in the …
[HTML][HTML] Impact of the diurnal cycle of solar radiation on intraseasonal SST variability in the western equatorial Pacific
T Shinoda - Journal of Climate, 2005 - journals.ametsoc.org
Impact of the Diurnal Cycle of Solar Radiation on Intraseasonal SST Variability in the
Western Equatorial Pacific in: Journal of Climate Volume 18 Issue 14 (2005) Jump to …
Western Equatorial Pacific in: Journal of Climate Volume 18 Issue 14 (2005) Jump to …
Observations of rain‐induced near‐surface salinity anomalies
Vertical salinity gradients in the top few meters of the ocean surface can exist due to the
freshwater input from rain. If present, surface gradients complicate comparing salinity …
freshwater input from rain. If present, surface gradients complicate comparing salinity …