slide 1/32noaa soil moisture/soil temperature workshop, oak ridge, tn, 3-5 march, 2009 value of...
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Slide 1/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
Value of Ground Network Observations in Value of Ground Network Observations in Development of Satellite Soil Moisture Development of Satellite Soil Moisture
Data ProductsData Products
X. ZhanX. Zhan11, J. Liu, J. Liu11, M. Cosh, M. Cosh22, T. Jackson, T. Jackson22,, andand Y. YuY. Yu11
1 1 NOAA-NESDIS Center for Satellite Applications and Research, Camp Springs, MDNOAA-NESDIS Center for Satellite Applications and Research, Camp Springs, MD22 USDA-ARS Hydrology and Remote Sensing Lab, Beltsville, MDUSDA-ARS Hydrology and Remote Sensing Lab, Beltsville, MD
Slide 2/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
OUTLINEOUTLINE
SatelliteSatellite SM data SM data
GroundGround SM and ST observations SM and ST observations
ResultsResults and and issuesissues in comparing them in comparing them
SuggestionsSuggestions for USCRN for USCRN
Slide 3/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
VUT ESCAT/ASCAT (Wagner et al, 1999)VUT ESCAT/ASCAT (Wagner et al, 1999)
USDA TMI (Bindlish et al, 2003)USDA TMI (Bindlish et al, 2003)
Princeton TMI (Gao et al, 2006)Princeton TMI (Gao et al, 2006)
NASA AMSR-E (Njoku et al, 2003)NASA AMSR-E (Njoku et al, 2003)
USDA AMSR-E (Jackson et al, 2007)USDA AMSR-E (Jackson et al, 2007)
VUA AMSR-E (Owe et al, 2008)VUA AMSR-E (Owe et al, 2008)
USDA WindSat (Jackson et al, 2008)USDA WindSat (Jackson et al, 2008)
NRL WindSat (Li et al, 2008)NRL WindSat (Li et al, 2008)
Satellite Soil Moisture Data Products:Satellite Soil Moisture Data Products:
Slide 4/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
USDA TMI (Bindlish et al, 2003)USDA TMI (Bindlish et al, 2003) ::
Daily Daily estimates, estimates,
from July 06 to from July 06 to July 21, 1999 July 21, 1999
0.0 – 0.52%v/v0.0 – 0.52%v/v
Slide 5/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
Princeton University TMI (Gao et al, 2006)Princeton University TMI (Gao et al, 2006) ::
Jan. 1, 1999 with quality masks appliedJan. 1, 1999 with quality masks applied
Slide 6/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
NASA AMSR-E (Njoku et al, 2003)NASA AMSR-E (Njoku et al, 2003) ::
Within US: Within US: 0.1 – 0.2 v/v0.1 – 0.2 v/v
Slide 7/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
VUA-GSFC AMSR-E (Owe et al, 2008)VUA-GSFC AMSR-E (Owe et al, 2008) ::
Monthly for Monthly for July 2003: July 2003:
Top: 6.9GHzTop: 6.9GHzBottom: 10.7 Bottom: 10.7
GHzGHz
Slide 8/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
USDA WindSat (Jackson et al, 2008)USDA WindSat (Jackson et al, 2008) ::
WindSat global WindSat global volumetric soil volumetric soil
moisture (%) for moisture (%) for July 30, 2005.July 30, 2005.
0.0 – 0.5 v/v0.0 – 0.5 v/v
Slide 9/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
NRL WindSat (Li et al, 2008)NRL WindSat (Li et al, 2008) ::
WindSat global volumetric soil moisture (%) and vegetation WindSat global volumetric soil moisture (%) and vegetation water content (kg/m2) retrievals for 1 – 12 September 2003.water content (kg/m2) retrievals for 1 – 12 September 2003.
Slide 10/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
MetOp ASCAT (Wagner et al, 1999)MetOp ASCAT (Wagner et al, 1999) ::
VUT ASCAT soil moisture is actually soil wetness, could be converted VUT ASCAT soil moisture is actually soil wetness, could be converted to volumetric soil moisture by dividing them with their soil porosityto volumetric soil moisture by dividing them with their soil porosity
Slide 11/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
Watershed SM Vitel Network (2001- present)Watershed SM Vitel Network (2001- present)
Soil Climate Analysis Network (1996- present)Soil Climate Analysis Network (1996- present)
Surface Radiation Budget Network (1993- present)Surface Radiation Budget Network (1993- present)
US Climate Reference Network (2002- present)US Climate Reference Network (2002- present)
Ground SM & ST Observations:Ground SM & ST Observations:
Slide 12/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
USDA-ARS Watershed SM Vitel Network:USDA-ARS Watershed SM Vitel Network:
LW: Little Washita, OK
WG: Walnut Gulch, AZ
AMSR-E U.S. Soil Moisture Validation SitesAMSR-E U.S. Soil Moisture Validation Sites
RC: Reynolds Creek, ID
LR: Little River, GA
Slide 13/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
USDA-ARS Watershed SM Vitel Network:USDA-ARS Watershed SM Vitel Network:
Multiple sites within Multiple sites within a satellite footprinta satellite footprint
Rain gauge overlay Rain gauge overlay SM sitesSM sites
Multiple layers (5cm, Multiple layers (5cm, 15cm, 30cm)15cm, 30cm)
Continuous data Continuous data sampling (30 min.)sampling (30 min.)
Stevens-Vitel Hydra Stevens-Vitel Hydra ProbesProbes
WG
LW
RC
LR
Slide 14/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
USDA-NRCS Soil Climate Analysis Network (SCAN):USDA-NRCS Soil Climate Analysis Network (SCAN):
Mostly single site in Mostly single site in a satellite footprinta satellite footprint
Rain gauge at the Rain gauge at the same sitesame site
Multiple layers (2”, Multiple layers (2”, 4”, 8”, 20”, 40”)4”, 8”, 20”, 40”)
Hourly dataHourly data
Hydra ProbesHydra Probes
Slide 15/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
NOAA Surface Radiation Budget Network (SurfRad):NOAA Surface Radiation Budget Network (SurfRad):
6 sites from 1995 6 sites from 1995 and 1 site from 2003and 1 site from 2003
Mainly solar and Mainly solar and thermal radiationthermal radiation
LST observational LST observational DataData
Sample per 1 or 3 Sample per 1 or 3 minutesminutes
Precision Precision Infrared Infrared RadiometerRadiometerss
Slide 16/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
NOAA Climate Reference Network (USCRN):NOAA Climate Reference Network (USCRN):
>100 stations with >100 stations with a few paired onesa few paired ones
Most climate Most climate variables variables including including precipitationprecipitation
SM/ST plannedSM/ST planned
SM/ST Sample SM/ST Sample freq ?freq ?
SM/ST sensors ?SM/ST sensors ?
Slide 17/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
Validating AMSR-E Soil Moisture Retrievals: Validating AMSR-E Soil Moisture Retrievals:
with with Watershed SM Vitel NetworkWatershed SM Vitel Network
(USDA-ARS)(USDA-ARS)
Slide 18/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
Validating AMSR-E Soil Moisture Retrievals: Validating AMSR-E Soil Moisture Retrievals:
with with SCAN Data SCAN Data (USDA-NRCS)(USDA-NRCS)
Slide 19/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
Validating Multiple Soil Moisture Retrievals: Validating Multiple Soil Moisture Retrievals:
with with SCAN Data SCAN Data (USDA-NRCS)(USDA-NRCS)
Slide 20/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
Evaluating LST Estimates (TEvaluating LST Estimates (Tskinskin) for SM Retrievals: ) for SM Retrievals:
TB,icmp= Tskin {er,p exp (-i/cos) +
(1 – ) [1 – exp (-i/cos)] [1 + Rr,i exp (-i/cos)]}
i = b *VWCRr,i = Rs exp(h cos2θ)
Rs = f(ε) -- Fresnel Equationε = g(SM) -- Mixing model
TB,iobs= TB06h , TB06v , TB10h , TB10v , TB18h , TB18v
}min{
26
1
,,2
i i
cmpiB
obsiB TT
Multi-channel Inversion (MCI) Algorithm (Njoku & Li, 1999):Multi-channel Inversion (MCI) Algorithm (Njoku & Li, 1999):
Slide 21/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
Evaluating LST Estimates (TEvaluating LST Estimates (Tskinskin) for SM Retrievals: ) for SM Retrievals:
TB10h = Ts [1 –Rr exp (-2 /cos)]
Rr = Rs exp(h cos2θ)
Rs = f(ε) -- Fresnel Equationε = g(SM) -- Mixing model
Ts = reg1(TB37v) or TsLSM
= b * VWCVWC = reg2(NDVI)
Single Channel Retrieval (SCR) Algorithm (Jackson, 1993):Single Channel Retrieval (SCR) Algorithm (Jackson, 1993):
Slide 22/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
Evaluating NCEP-GDAS TEvaluating NCEP-GDAS Tskinskin Estimates: Estimates:
with with SurfRadSurfRad(NOAA)(NOAA)
Slide 23/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
Evaluating NCEP-GDAS TEvaluating NCEP-GDAS Tskinskin Estimates: Estimates:
with with SurfRadSurfRad(NOAA)(NOAA)
Slide 24/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
Evaluating NCEP-GDAS TEvaluating NCEP-GDAS Tskinskin Estimates: Estimates:
with with SurfRadSurfRad(NOAA)(NOAA)
Slide 25/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
Evaluating TEvaluating Tskinskin Estimates from AMSR-E TB36v: Estimates from AMSR-E TB36v:
Slide 26/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
Evaluating TEvaluating Tskinskin Estimates from AMSR-E TB36v: Estimates from AMSR-E TB36v:
Slide 27/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
Evaluating TEvaluating Tskinskin Estimates from AMSR-E TB36v: Estimates from AMSR-E TB36v:
Slide 28/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
Issues in Satellite SM Validation with in situ Data: Issues in Satellite SM Validation with in situ Data:
1.1. Footprint Footprint representation/ representation/ heterogeneity heterogeneity issueissue
Slide 29/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
Issues in Satellite SM Validation with in situ Data: Issues in Satellite SM Validation with in situ Data:
2.2. Hydra probe depth Hydra probe depth vs vs satellite sensor depthsatellite sensor depth
SCAN probe depth:SCAN probe depth:2”, 4”, 8”, 20”, 40”2”, 4”, 8”, 20”, 40”
USDA Vitel Network:USDA Vitel Network:5cm, 15cm, 30cm5cm, 15cm, 30cm
Noah LSM depth: 10cm, Noah LSM depth: 10cm, 40cm, 100cm, 200cm 40cm, 100cm, 200cm
AMSR-E (C-band) AMSR-E (C-band) sensible depth: < 2cmsensible depth: < 2cm
SMAP (L-band): < 5cmSMAP (L-band): < 5cm
USCRN: ?USCRN: ?
Slide 30/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
Issues in Satellite SM Validation with in situ Data: Issues in Satellite SM Validation with in situ Data:
3.3. Hydra Probe Hydra Probe calibration calibration standardizationstandardization
Slide 31/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
Representation issue:Representation issue: Identify those sites with good Identify those sites with good area landscape heterogeneity for SM/ST sensor area landscape heterogeneity for SM/ST sensor installation if not all sites;installation if not all sites;
Probe depth issue: Probe depth issue: Consider future operational or long Consider future operational or long term C/X-band satellite sensors (MIS, AMSR2, GPM, term C/X-band satellite sensors (MIS, AMSR2, GPM, etc) as well as L-band sensors (SMOS, SMAP);etc) as well as L-band sensors (SMOS, SMAP);
Data quality issue:Data quality issue: Plan frequent sensor calibration Plan frequent sensor calibration based on timely data analysis;based on timely data analysis;
LST (TLST (Tskinskin): ): LST observations are desirable for both LST observations are desirable for both
satellite (SM/ST) data products validation and climate satellite (SM/ST) data products validation and climate monitoring;monitoring;
Data access: Data access: Open, timely, and convenient access to Open, timely, and convenient access to USCRN data benefits all of their potential applications USCRN data benefits all of their potential applications (drought monitoring, satellite data validation, etc)(drought monitoring, satellite data validation, etc)
SUGGESTIONS FOR USCRNSUGGESTIONS FOR USCRN
Slide 32/32NOAA Soil Moisture/Soil Temperature Workshop, Oak Ridge, TN, 3-5 March, 2009
Currently availableCurrently available satellite SM data products satellite SM data products are are significantly differing from each other and their qualities significantly differing from each other and their qualities need to be improved for operational uses;need to be improved for operational uses;
SM ground measurements SM ground measurements are useful for satellite SM/ST are useful for satellite SM/ST data product validation and verification of land surface data product validation and verification of land surface model SM/ST data assimilation;model SM/ST data assimilation;
There are spaces for improving the ground SM/ST There are spaces for improving the ground SM/ST measurement qualitymeasurement quality with consideration to satellite with consideration to satellite footprint representation, sensor depth, calibration footprint representation, sensor depth, calibration standardization and open, timely, convenient data access;standardization and open, timely, convenient data access;
In addition to soil temperature measurements, In addition to soil temperature measurements, Land Land Surface Temperature (TSurface Temperature (Tskinskin)) observations are also observations are also
desirable for satellite (SM/ST) data product validations;desirable for satellite (SM/ST) data product validations;
SUMMARYSUMMARY