2019 User Working Group (UWG) Meeting
PO.DAAC welcomed our UWG, other DAAC representatives, and NASA officials for the annual meeting on 25-26 June 2019.
PO.DAAC welcomed our UWG, other DAAC representatives, and NASA officials for the annual meeting on 25-26 June 2019.
The World Data System (WDS), an international consortium promoting scientific data integrity, trust and stewardship, has recognized the PO.DAAC as a data center meeting the requirements of the CoreTrustSeal (https://www.coretrustseal.org/) . This universal catalogue of criteria reflects the core characteristics of trustworthy data repositories and indicates that the PO.DAAC meets the highest international requirements for quality assured scientific data and services, and data archiving and stewardship.
Suresh Vannan, Mike Gangl and Jessica Hausman representing PO.DAAC at the Surface Water and Ocean Topography (SWOT) Science Team Meeting in Bordeaux, France.
Correction: The release of GRACE-FO Level 2 RL06 contains the 9 monthly gravity field coefficient datasets from June-2018 through Apr-2019, Including [06, 07, 10, 11, 12]-2018 and [01, 02, 03, 04]-2019.
The Gravity Recovery and Climate Experiment Follow-On (GRACE-FO) mission, a joint partnership between NASA and the German Research Centre for Geosciences (GFZ), launched on 22 May 2018. It uses twin satellites to accurately map variations in the Earth's gravity field and surface mass distribution. It is designed as a successor to the Gravity Recovery and Climate Experiment (GRACE) mission.
Conceptually very similar to the original GRACE mission (2002 – 2017), GRACE-FO consists of two identical satellites flying in formation around Earth at an initial altitude of approximately 490 kilometers and a nominal separation distance of 220+/-50 kilometers. Instruments on board the satellites precisely measure changes in the distance between them due to orbital perturbations caused by geographical and temporal variations in Earth's gravity field.
GRACE-FO will expand GRACE's legacy of scientific achievements. These include tracking mass changes in Earth's polar ice sheets and mountain glaciers (which impacts global sea level); estimating total water storage on land (from groundwater changes in deep aquifers to changes in soil moisture and surface water); inferring changes in deep ocean currents, a driving force in climate; and even measuring changes within the solid Earth itself, such as postglacial rebound and the impact of major earthquakes.
GRACE-FO mission datasets are archived and distributed by the PO.DAAC. The datasets are described and discoverable via the PO.DAAC dataset information pages. The dataset information pages also provide access to the technical documentation, GRACE-FO Level-2 User Handbook, and guidance on how to cite the data.
The 2018 Atlantic hurricane season featured 15 named storms. The season officially began on 25 May 2018 with the formation of Tropical Storm Alberto and ended on 31 October 2018 with the dissipation of Hurricane Oscar.
Evolution of GOES-East IR, NASA Soil Moisture Active Passive (SMAP) sea surface salinity (SSS), and NASA Multi-Scale Ultra-High Resolution (MUR) sea surface temperature (SST) response to the 2018 Atlantic hurricane season response. (MUR SST DOI: 10.5067/GHGMR-4FJ04; SMAP SSS DOI: 10.5067/SMP42-3TPCS).
Evolution of the NASA Soil Moisture Active Passive (SMAP) sea surface salinity (SSS) response to the 2018 Atlantic hurricane season. It is common to observe patches of 1) salinity freshening due to enhanced precipitation and 2) salinity increase due to wind stress-generated vertical mixing, wherein increased salinity from a mid-level maximum is brought to the surface. The two effects are clearly observed along the tracks of the 2018 Atlantic tropical cyclones. (SMAP SSS DOI: 10.5067/SMP42-3TPCS).
Evolution of the NASA Multi-Scale Ultra-High Resolution (MUR) sea surface temperature (SST) response to the 2018 Atlantic hurricane season. It is common to observe trails of cooler water, or cold wakes, along hurricane tracks as a result of wind-induced mixing and turbulence that brings cold waters at depth to the surface. The cold wakes associated with the 2018 Atlantic tropical cyclones are clearly observed as waters approximately 2°C cooler from normal that persisted for several days. (MUR SST DOI: 10.5067/GHGMR-4FJ04).
DOI MBES: 10.5067/OMGEV-MBES1
DOI SBES: 10.5067/OMGEV-SBES1