Data in Action: GRACE – Uncovering the 2010-11 decline in global mean sea level and its relation to ENSO

In mid 2010 to mid 2011, global mean sea level (GMSL) dropped by ~5 mm. By “weighing“ the ocean using the Gravity Recovery And Climate Experiment (GRACE) satellites, the source of this sudden decrease can be determined. Was there less water in the ocean or was it temporarily cooler than normal?

SPURS Sets Sail to Elucidate Oceanic Salinity Processes with Linkage to the Water Cycle (September, 2012)

Funded by NASA in collaboration with NSF, NOAA and also involving European participation (e.g. France, Spain), the Salinity Processes in the Upper Ocean Regional Study (SPURS) project aims to improve our understanding of salinity processes in the upper ocean. Along with the AQUARIUS/SAC-D mission, a collaboration between NASA and the Argentinian Space Agency CONAE, SPURS will provide new insights into the Earth's global water cycle and the relationship to climate. AQUARIUS data is available through the PO.DAAC. 

Data in Action: SPURS Sets Sail to Elucidate Oceanic Salinity Processes with Linkage to the Water Cycle

Final preparations of the research vessel (R/V) Knorr are underway at the Woods Hole Oceanographic Institute for one of a series of 5 cruises during 2012 and 2013 that are part of an innovative research program called SPURS. Funded by NASA in collaboration with NSF, NOAA and also involving European participation (e.g. France, Spain), the Salinity Processes in the Upper Ocean Regional Study (SPURS) project aims to improve our understanding of salinity processes in the upper ocean.

Gridded Climate Variables for Model Intercomparison

September 13, 2012

PO.DAAC is pleased to announce that it will distribute three gridded satellite datasets to facilitate climate model evaluation. They include variables for Sea Surface Temperature (SST), Absolute Dynamic Topography (ADT), and ocean surface vector winds.   These observational datasets are on monthly 1° grids with various time series lengths.  They were generated with the initial intention to facilitate the intercomparison of satellite derived observations with climate model outputs from CMIP5 (Coupled Model Intercomparison Project Phase 5) under the World Climate Research Program (WCRP).  However, their utility extends beyond climate model evaluation.  Each climate variable contains the data, number of observations, and the standard deviation for each bin on the grid.  Documentation and read software are available for these datasets in the same location as the data.  The documentation explains the contents of the dataset, how it was calculated and how the errors were calculated. All of these datasets are available via OPeNDAP, THREDDS (see below for links), and LAS.  LAS is the Live Access Server that allows for visualization, subsetting, and cursory analysis.  LAS is located at https://podaac-tools.jpl.nasa.gov/las/.

The SST (fig. 1) dataset is derived from the Advanced Microwave Scanning Radiometer (AMSR-E) instrument onboard the NASA Aqua satellite, a passive-microwave radiometer that sees through most clouds, and was created by Remote Sensing Systems.  The data start in July 2002 and end December 2010.


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                                                      Figure 1. AMSR-E SST from the month of April 2009.

ADT, the sea surface height relative to the geoid (the mean ocean surface of the Earth if the ocean is at rest) (fig. 2), is derived from TOPEX/Poseidon, Envisat, Jason-1, and OSTM/Jason-2.  This dataset was generated by AVISO.  The data start in October 1992 and end in December 2010.

 


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                                                   Figure 2.:  ADT during April 2009, blended from TOPEX/Poseidon, Envisat, Jason-1 and/or OSTM/Jason-2.

Ocean surface vector winds (fig. 3) are derived from the NASA QuikSCAT mission and contain wind speed, and meridional and zonal wind vector components.  This dataset was created by the QuikSCAT project at Jet Propulsion Laboratory.  The data start in August 1999 and end in October 2009.

  • Dataset information pages: 

https://podaac.jpl.nasa.gov/dataset/QSCAT_L3_SFC_WIND_SPEED_1DEG_1MO
https://podaac.jpl.nasa.gov/dataset/QSCAT_L3_SFC_EASTWARD_WIND_1DEG_1MO
https://podaac.jpl.nasa.gov/dataset/QSCAT_L3_SFC_NORTHWARD_WIND_1DEG_1MO

 
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                                                    Figure 3.: QuikSCAT wind speed during September 2005.

 

Data in Action: Aquarius reveals salinity structure of tropical instability waves

Tropical Instability Waves (TIWs) are westward-traveling waves associated with shear instabilities of the equatorial current system, and are observed at the edges of the equatorial cold tongues in the Pacific and Atlantic Oceans. TIWs have average wavelengths of 1000-2000 kilometers, periods of 20-40 days, and phase speeds of 0.3-0.5 m/s. These waves redistribute various ocean properties, including temperature, salinity, and nutrients.

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