land surface modeling studies in support of aqua amsr-e validation

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Land Surface Modeling Studies in Support of AQUA AMSR-E Validation PI: Eric F. Wood, Princeton University Project Goal: To provide modeling support to the AMSR-E validation activities through a combination of soil moistures retrievals (using the Princeton (PU) Land Surface Microwave Emission Model (LSMEM) and process-based hydrological modeling. Recent Activities: 1. Validation using SMEX02/03, NAME, and OK- mesonet data 2. Comparisons between AMSR-E and TMI over OK region Princeton University

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Land Surface Modeling Studies in Support of AQUA AMSR-E Validation PI: Eric F. Wood, Princeton University. Princeton University. Project Goal: - PowerPoint PPT Presentation

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Page 1: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

PI: Eric F. Wood, Princeton University

Project Goal:

To provide modeling support to the AMSR-E validation activities

through a combination of soil moistures retrievals (using the

Princeton (PU) Land Surface Microwave Emission Model

(LSMEM) and process-based hydrological modeling.

Recent Activities:

1. Validation using SMEX02/03, NAME, and OK-mesonet data

2. Comparisons between AMSR-E and TMI over OK region

Today FocusIntercomparison of two AMSR-E soil moisture retrievals algorithms

and their validation.Princeton University

Page 2: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

Basis of the validation research

Princeton University

1. Soil moisture retrievals used the Princeton (PU) Land Surface Microwave Emission Model (LSMEM) and 10.7 GHz brightness temperatures from the TRMM Microwave Imager (TMI) and AMSR-E. LSMEM is based on Tb(H) and Ts, plus ancillary land surface data (soil, vegetation, etc.)

2. Retrieval comparisons were with a JPL-version of the AMSR-E retrieval algorithm for TMI and the NASA/AMSR-E 10.7 GHz retrievals; these use a polarization ratio approach and empirical parameters.

3. Comparisons were also made to SMEX field data, 5-cm soil moisture from 30 Oklahoma mesonet data sites, and to 10-cm soil moisture from a land surface model.

Page 3: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

SMEX02: PU/AMSR-E X-Band Soil Moisture Comparison with the ARS SCAN Soil Moisture Monitoring Site

Princeton University

Page 4: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

SMEX02: PU/AMSR-E 10.7 GHz Soil Moisture Comparison with the Theta Probe Field Data

Princeton University

Date Samples Soil Moisture PU/Avg Std dev AMSR*

6-25 272 12.8 2.6 9.56-26 273 12.1 2.8 6-27 273 11.3 2.3 7.07-1 103 9.5 1.6 8.57-5 271 14.8 2.4 7-6 273 14.4 2.2 14.07-7 273 18.4 2.7 28.5 7-8 273 16.6 2.3 17.07-9 273 15.3 2.4 17.07-11 260 26.4 1.8 26.57-12 273 25.2 2.1

*AMSR-E values indicate the resampled pixel that encompasses the Walnut Creek catchment ~65% of the pixel

Page 5: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

SMEX02: PU/AMSR-E X-Band Soil Moisture Comparison with the Field Theta Probe Measurements

Princeton University

(Notice how PU/AMSR-E has more realistic variability after rain events)

(Theta Probe data)

Page 6: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

June 26

July 5

July 19

June 27 - 25

July 6 – 4

July 20 – 18

Rainfall and Retrieved PU/AMSR soil moisture patterns

Princeton University

Dynamic range +/- 20%

Page 7: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

PU/AMSR

NASA/AMSR

Princeton University

NASA/AMSR-E has significantly reduced dynamic range when compared to PU/AMSR-E. Because of scale effects IT IS IMPOSSIBLE TO RESOLVE (VALIDATE) WHICH IS CORRECT. Therefore we must consider statistical consistency between satellite and in-situ observations.

Page 8: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

Rainfall (mm)

Princeton University

Looking at soil moisture differences between pre- and post-rain days

PU/AMSR-E differences % soil moisture

NASA/AMSR-E differences – reduced range

Page 9: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

AMSR-E Near Surface Soil Moisture

AMSR-E retrieved soil moisture represents surface wetness (~0.5cm) and tends to have much lower mean soil moisture but good dynamic range.

Princeton University

Page 10: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

Soil Moisture – Rainfall Comparison

Precipitation Aug 29/31:

…strong influence on soil storage in both the VIC and AMSR responses.

Delayed response evident in VIC estimates.

Princeton University

Soil moisture

PU/AMSR

10-cm LSM

Page 11: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

Algorithm Validation/Comparisons over the SGP

Princeton University

Used 6 years of TMI 10.7 GHz data (1998-2003) and 2 years of AMSR-E data (2003-2004).

With TMI, used JPL/TMI algorithm from Eni Njoku. With AMSR-E, used retrieved soil moisture from the NASA DAAC.

Page 12: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

AMSR-E retrieved soil moisture July 23, 2002

TMI retrieved soil moisture July 25, 2002

PU/AMSR-E 10.7 GHz Soil Moisture Comparisons with PU/TMI-based Soil Moisture

Princeton University

AMSR-E retrieved soil moisture July 25, 2002

TMI retrieved soil moisture July 23, 2002

Page 13: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

AMSR-E, TMI OK-Mesonet VIC/LSM

AMSR-E soil moisture (%)T

MI s

oil

mo

istu

re (

%)

PU/AMSR-E X-Band Soil Moisture Comparisons with PU/TMI X-Band Soil Moisture

Princeton University

Lesson: Retrievals consistent across sensors, but different from in-situ

Page 14: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

Retrieved soil moisture averaged over 30 Oklahoma mesonet sites

Princeton University

Soil moisture using PU LSMEM algorithm

30-s

ite

OK

-mes

on

et s

oil

mo

istu

re

Soil moisture using NASA/JPL algorithm

30-s

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-mes

on

et s

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re

Princeton University

Page 15: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

So

il m

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TMI

Soil moisture using PU LSMEM algorithm

Algorithm comparison for retrieved soil moisture averaged over 30 Oklahoma mesonet sites

Princeton University

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Soil moisture using PU LSMEM algorithm

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Page 16: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

Princeton University

Model vs PU/TMI Model vs OK-mesonet

Comparisons between LSM and retrieved soil moistures

Model vs JPL/TMI

Page 17: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

Princeton University

Statistical consistency between LSM and retrieved soil moistures

Page 18: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

AMSR-E results from PU/LSMEM (left) and NASA/DAAC (right)for 2004 AMSR-E am overpasses over the 30 OK-mesonet sites, compared to the 30 mesonet sites

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Mesonet-Daily

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Mesonet-Daily

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-AM

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Princeton University

Page 19: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

AMSR-E results from PU/LSMEM (left) and NASA/DAAC (right)for 2004 am overpasses over the 30 OK-mesonet sitescompared with the same sites from VIC 2am LSM output.Parabolic trend line has been fitted to both; Note that rainfall has been filtered out of the LSMEM result but not the NASA/DAAC

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Princeton University

Page 20: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

Implications for retrieval error estimates and use in assimilation

1. The reality that retrieved soil moistures have different mean values and dynamic ranges implies that new, innovative statistical approaches are needed for validation: “statistical consistency” – this is currently being developed at Princeton.

2. The lack of a dynamic range in the NASA/JPL DAAC algorithms is problematic, but the two products are well correlated.

3. Sensitivity analysis for the algorithms are underway. For the PU LSMEM, errors in Ts appear to result in high frequency noise in SM during dry periods.

4. For individual (validation) points, the errors between satellite retrievals (at 25-40 km scales) can be very large.

Princeton University

Page 21: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

Sensitivity of retrieved soil moisture using the PU LSMEM uncertainty in Ts (RMS error 3K) for four OK-mesonet sites (i.e. soil, vegetation, roughness characteristics from the sites)

Ret

riev

ed s

oil

mo

istu

re

‘Observed’ 10.7 GHz brightness temperatures: Tb(V)—red; Tb(H)—black(results from 100 Monte Carlo simulations)

Princeton University

Page 22: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

Comparisons between observed and simulated Tb, over 23 OK-mesonet sites, for 363 TMI orbits from 2003

Princeton University

Page 23: Land Surface Modeling Studies in Support of AQUA AMSR-E Validation

Princeton University

Comparisons between observed and simulated Tb, averaged over 23 OK-mesonet sites, for 363 TMI orbits from 2003