Evaluation of sea surface salinity observed by Aquarius and SMOS



Similar documents
Data Assimilation and Operational Oceanography: The Mercator experience

Satellite SST Product Development Proposal

Coriolis data-centre an in-situ data portail for operational oceanography.

Daily High-resolution Blended Analyses for Sea Surface Temperature

Huai-Min Zhang & NOAAGlobalTemp Team

IMPACTS OF IN SITU AND ADDITIONAL SATELLITE DATA ON THE ACCURACY OF A SEA-SURFACE TEMPERATURE ANALYSIS FOR CLIMATE

Near Real Time Blended Surface Winds

Coriolis data centre Coriolis-données

COASTAL WIND ANALYSIS BASED ON ACTIVE RADAR IN QINGDAO FOR OLYMPIC SAILING EVENT

hydrographic variability from Argo, SST and altimeter observations

HFIP Web Support and Display and Diagnostic System Development

Develop a Hybrid Coordinate Ocean Model with Data Assimilation Capabilities

The relationships between Argo Steric Height and AVISO Sea Surface Height

Coriolis, a French project for operational oceanography

Baudouin Raoult, Iryna Rozum, Dick Dee

GLOBAL TEMPERATURE AND SALINITY PROFILE PROGRAMME (GTSPP) Dr. Charles Sun, GTSPP Chair National Oceanographic Data Center USA

The impact of window size on AMV

CLIMATOLOGICAL DATA FROM THE WESTERN CANADIAN ODAS MARINE BUOY NETWORK

TROPICAL ATMOSPHERE-OCEAN (TAO) PROGRAM FINAL CRUISE REPORT TT Area: Equatorial Pacific: 8 N 95 W to 8 S 95 W and 8 S 110 W to 8 N 110 W

A beginners guide to accessing Argo data. John Gould Argo Director

A view of Earth, the Blue Planet, taken from Apollo 17 in 1972 (NASA)

WOCE Global Data. Version 3.0, 2002 ROM

Scholar: Elaina R. Barta. NOAA Mission Goal: Climate Adaptation and Mitigation

CTD Oceanographic Tags

Ocean Level-3 Standard Mapped Image Products June 4, 2010

Integrated Global Carbon Observations. Beverly Law Prof. Global Change Forest Science Science Chair, AmeriFlux Network Oregon State University

Paul S. Chang, Zorana Jelenak, Seubson Soisuvarn Faozi Said NOAA/NESDIS/STAR. Many thanks to the JPL/NASA RapidScat Team

Data Management Handbook

DELAYED MODE QUALITY CONTROL OF ARGO SALINITY DATA IN THE MEDITERRANEAN AND BLACK SEA FLOAT WMO G. Notarstefano and P.-M.

Clear Sky Radiance (CSR) Product from MTSAT-1R. UESAWA Daisaku* Abstract

MI oceanographic data

Long-term Marine Monitoring in Willapa Bay. WA State Department of Ecology Marine Monitoring Program

SATELLITE OCEANOGRAPHY IN THE AZORES: PAST, PRESENT AND FUTURE

User Perspectives on Project Feasibility Data

Survey Sensors Hydrofest Ross Leitch Project Surveyor

The Copernicus Marine Enviroment Monitoring Service

Marine route optimization. Jens Olaf Pepke Pedersen Polar DTU / DTU Space

Present Status of Coastal Environmental Monitoring in Korean Waters. Using Remote Sensing Data

Malcolm L. Spaulding Professor Emeritus, Ocean Engineering University of Rhode Island Narragansett, RI 02881

The MONGOOS Data portal EMODNET ROOS meeting, Brussels, 18 November 2013

Improving Accuracy of Solar Forecasting February 14, 2013

World Ocean Atlas (WOA) Product Documentation

Development of an Integrated Data Product for Hawaii Climate

ICES Guidelines for Profiling Float Data (Compiled January 2001; revised April 2006)

Dynamics IV: Geostrophy SIO 210 Fall, 2014

Real-time Ocean Forecasting Needs at NCEP National Weather Service

Improved Meteorological Measurements from Merchant Ships. Peter K. Taylor and Elizabeth C. Kent Southampton Oceanography Centre, UK

Estimating Firn Emissivity, from 1994 to1998, at the Ski Hi Automatic Weather Station on the West Antarctic Ice Sheet Using Passive Microwave Data

A METHODOLOGY FOR GIS INTERFACING OF MARINE DATA

IOC-UNESCO Regional Training Centre for the OceanTeacher Global Academy

Developing Continuous SCM/CRM Forcing Using NWP Products Constrained by ARM Observations

Jason-2 GDR Quality Assessment Report. Cycle / M. Ablain, CLS. P. Thibaut, CLS

Finnish Marine Research Infrastructure FINMARI

Parameterization of Cumulus Convective Cloud Systems in Mesoscale Forecast Models

SPATIAL DISTRIBUTION OF NORTHERN HEMISPHERE WINTER TEMPERATURES OVER THE SOLAR CYCLE DURING THE LAST 130 YEARS

Jason-2 GDR Quality Assessment Report. Cycle / S. Philipps, CLS. M. Ablain, CLS. P. Thibaut, CLS

Satellite Derived Dynamic Ocean Currents in the Arctic. Jens Olaf Pepke Pedersen Polar DTU / DTU Space

Mission Operations and Ground Segment

CCAR Near Real Time and Historical Altimeter Data Server

New Release of Satellite Turbulent Fluxes

Oceanographic quality flag schemes and mappings between them

A comparison of NOAA/AVHRR derived cloud amount with MODIS and surface observation

Very High Resolution Arctic System Reanalysis for

Ensuring the Preparedness of Users: NOAA Satellites GOES R, JPSS Laura K. Furgione

Monitoring Soil Moisture from Space. Dr. Heather McNairn Science and Technology Branch Agriculture and Agri-Food Canada

REDUCING UNCERTAINTY IN SOLAR ENERGY ESTIMATES

PE s Research activities and potential links to MM5. Red Ibérica MM5 Valencia 9th -10th June 2005

Maintenance and Disposition. Ocean and Marine Technology Functional Files. Function Number 1800

Intra-seasonal and Annual variability of the Agulhas Current from satellite observations

An improved correction method for high quality wind and temperature observations derived from Mode-S EHS

The Soil Moisture and Ocean Salinity Mission

Transcription:

SMOS & Aquarius science workshop (April 17, 2013) Evaluation of sea surface salinity observed by Aquarius and SMOS Hiroto Abe, Naoto Ebuchi (Hokkaido University, Japan) 1

Introduction (1/1) Aquarius V2.0 has been opened to the public. Other SSS products also have been produced, based on different algorisms (e.g. Combined-Active-Passive (NASA/JPL)) and different measurement (SMOS). Evaluations of these products based on in situ observations are needed to reveal their accuracies and error structures. Objective of this study Evaluate SSS observed by Aquarius and SMOS including their error structures. 2

Data (1/1) - Level 2 - Satellite salinity Aquarius SSS (beam1) 1) V2.0 : NASA/JPL PO.DAAC 2) CAP V2.0 : NASA/JPL Dr. Simon Yueh 3) RSS testbed : Remote Sensing Systems (galaxy correction done) In situ salinity 1) Argo salinity : Global Data Assembly Center, realtime mode data 2) TAO/TRITON, PIRATA, RAMA buoys 3

Comparison to in situ data (1/3) Argo vs AQ V2.0 Scatter plot of collocated data Aquarius V2.0 (psu) V2.0 Argo salinity (psu) Period : 25 Aug 2011 31 Dec 2012 Matchup condition : 200 km, 12 h 1) wind speed < 15m/s 2) Argo temperature > 5C 3) Argo depth < 12.5 dbar 4) rad_land_frac < 0.0005 5) rad_ice_frac < 0.0005 bias:-0.02 psu Standard deviation (stddev) :0.58 psu 4

Comparison to in situ data (2/3) Argo vs AQ Scatter plot of collocated data V2.0 CAP V2.0 RSS testbed Aquarius V2.0 (psu) Argo salinity (psu) bias: -0.02 psu -0.06 0.00 stddev: 0.58 0.57 0.44 Standard deviation is large in this order V2.0 > CAP 2.0 > RSS testbed 5

Comparison to in situ data (3/3) Mooring buoy (1 dbar) vs AQ Scatter plot of collocated data V2.0 CAP V2.0 RSS testbed Aquarius V2.0 (psu) Argo salinity (psu) bias: -0.01 psu -0.02 0.00 stddev: 0.48 0.47 0.41 The order does not change 6

Error structure (1/3) ~SST~ V2.0 residual 2-2 0 CAP V2.0 0 10 20 30 bias 0.5 0.0-0.5 stddev Residual analysis 10 20 30 RSS testbed Argo temperature( ) 1.0 0.0 Argo temperature( ) The smallest stddev is found in RSS testbed. 7

Error structure (2/3) ~wind speed~ V2.0 residual 2-2 0 CAP V2.0 0 10 20 bias 0.5 0.0-0.5 stddev Residual analysis 10 20 RSS testbed Wind speed (m/s) 1.0 0.0 Wind speed (m/s) The stddev in RSS testbed is the smallest. 8

Error structure (3/3) ~SST and wind speed~ Wind speed (m/s) stddev V2.0 CAP V2.0 RSS testbed Argo temperature( ) 1.2 0.8 0.4 0.0 Stddev (psu) 1) V2.0 has large stddev under low SST and high wind speed conditions. 2) The contrast is strong for stddev in CAP V2.0. 3) Wind speed dependency is weak for stddev in RSS testbed. 9

Ascending minus descending seasonality (1/2) Ascending descending V2.0 CAP V2.0 RSS testbed -0.8 0.0 +0.8 10

V2.0 Ascending minus descending seasonality (2/2) 60N latitude 0 60S CAP V2.0 S N J M M J S N Ascending descending (latitude-time diagram) (psu) +0.8 0.0 2011 2012 RSS testbed -0.8 SSS bias between ascending and descending is improved for RSS testbed. However, it still remains. 11

Data (1/1) - Level 3 - Satellite salinity 1) Aquarius Level 3 V2.0 SSS : NASA/JPL PO.DAAC 2) SMOS Level 3 reprocessed SSS : CATDS, CNES Salinity data 1) Argo optimal interpolation : JAMSTEC (MOAA GPV) (Argo salinities are interpolated based on World Ocean Atlas 2001 as the first guess) 2) Assimilation data system : Japan Meteorological Research Institute (MRI) (In-situ and satellite altimeter data are assimilated. Combination of OGCM and EOF) 12

Comparison to monthly JAMSTEC Argo OI (1/3) Aquarius V2.0 Aquarius V2.0 v.s. JAMSTEC Argo OI (March 2012) Aquarius V2.0 JAMSTEC Argo OI JAMSTEC Argo OI (10m) Stddev is 0.38 psu (>0.2 psu) Residual SSS are negative 1) low latitude 2) Kuroshio and Gulf stream 13

Comparison to monthly JAMSTEC Argo OI (2/3) SMOS SMOS v.s. JAMSTEC Argo OI (March 2012) SMOS JAMSTEC Argo OI JAMSTEC Argo OI (10m) 14

Comparison to monthly JAMSTEC Argo OI (3/3) Stddev of residual SSS (psu) (40S-40N) 2011 2012 Aquarius 0.33 psu < SMOS 0.35 psu 15

Comparison to J-MRI assimilation system (1/3) Aquarius V2.0 Aquarius V2.0 v.s. J-MRI assimilation (March 2012) Aquarius V2.0 MRI assimilation SSS MRI assimilation SSS (1m) 16

Comparison to J-MRI assimilation system (2/3) SMOS SMOS v.s. J-MRI assimilation (March 2012) SMOS MRI assimilation SSS MRI assimilation SSS (1m) 17

Comparison to J-MRI assimilation system (3/3) Stddev of residual SSS (psu) (40S-40N) 2011 2012 Aquarius 0.36 psu < SMOS 0.39 psu 18

Summary (1/2) Aquarius and SMOS SSSs were evaluated. Level 2 (Aquarius) Stddev of residual SSS using Argo ranged from 0.44-0.58 psu. Stddev in RSS testbed was the smallest The stddev showed different error structures. 1) V2.0 : large stddev under low SST and high wind speed. 2) CAP V2.0 : the contrast was strong. 3) RSS testbed : weak dependency for wind speed. Ascending and descending bias was improved for RSS testbed. However it was not removed completely. 19

Summary (2/2) Level 3 (Aquarius and SMOS) Stddev of the residual for the Aquarius SSS was smaller than that of SMOS. JAMSTEC Argo OI : 0.33 psu (AQ) and 0.35 psu (SMOS) J-MRI assimilation : 0.36 psu (AQ) and 0.39 psu (SMOS) Acknowledgment We would like to thank all the data provider! 20