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Sensitivity of multi-parameter soil moisture retrievals to incidence angle configuration

Identifieur interne : 005A22 ( PascalFrancis/Curation ); précédent : 005A21; suivant : 005A23

Sensitivity of multi-parameter soil moisture retrievals to incidence angle configuration

Auteurs : Sandy Peischl [Australie] ; Jeffrey P. Walker [Australie] ; NAN YE [Australie] ; DONGRYEOL RYU [Australie] ; Yann Kerr [France]

Source :

RBID : Pascal:14-0131784

Descripteurs français

English descriptors

Abstract

This paper focuses on the sensitivity of L-band multi-parameter retrievals across the range of angular measurements available from the SMOS (Soil Moisture and Ocean Salinity) mission. The SMOS core algorithm was used to evaluate two-parameter retrieval scenarios including soil moisture and one of either i) vegetation water content, ii) surface roughness, iii) vegetation temperature, or iv) surface soil temperature. For all pairs a range of parameter value combinations were compiled to run the model in forward mode. Subsequently, the resulting angular brightness temperature simulations with two unknown parameters were compared against the brightness temperature response derived from reference simulations using data from the National Airborne Field Experiment 2005 (NAFE'05) in Australia. This paper showed that the two-parameter retrieval accuracy of soil moisture is strongly affected by the surface moisture conditions, the polarization of the brightness temperature data, and the choice of the secondary ancillary parameter to be retrieved. The synthetic analysis demonstrated a tendency for better retrievals from dual-polarized data at large incidence angles (40-50°). Validation with airborne brightness temperature observations at L-band did not demonstrate such a strong angular dependency, although it confirmed that the simultaneous retrieval of soil moisture and vegetation properties is not preferable as opposed to i) soil moisture and surface roughness or ii) soil moisture and surface soil temperature, especially under dry moisture conditions.
pA  
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A03   1    @0 Remote sens. environ.
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A08 01  1  ENG  @1 Sensitivity of multi-parameter soil moisture retrievals to incidence angle configuration
A11 01  1    @1 PEISCHL (Sandy)
A11 02  1    @1 WALKER (Jeffrey P.)
A11 03  1    @1 NAN YE
A11 04  1    @1 DONGRYEOL RYU
A11 05  1    @1 KERR (Yann)
A14 01      @1 Department of Civil Engineering, Monash University @3 AUS @Z 1 aut. @Z 2 aut. @Z 3 aut.
A14 02      @1 Department of Infrastructure Engineering, The University of Melbourne @3 AUS @Z 4 aut.
A14 03      @1 Centre d'Etudes Spatiales de la Biosphere (CESBIO) @2 Toulouse @3 FRA @Z 5 aut.
A20       @1 64-72
A21       @1 2014
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A47 01  1    @0 14-0131784
A60       @1 P
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A64 01  1    @0 Remote sensing of environment
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C01 01    ENG  @0 This paper focuses on the sensitivity of L-band multi-parameter retrievals across the range of angular measurements available from the SMOS (Soil Moisture and Ocean Salinity) mission. The SMOS core algorithm was used to evaluate two-parameter retrieval scenarios including soil moisture and one of either i) vegetation water content, ii) surface roughness, iii) vegetation temperature, or iv) surface soil temperature. For all pairs a range of parameter value combinations were compiled to run the model in forward mode. Subsequently, the resulting angular brightness temperature simulations with two unknown parameters were compared against the brightness temperature response derived from reference simulations using data from the National Airborne Field Experiment 2005 (NAFE'05) in Australia. This paper showed that the two-parameter retrieval accuracy of soil moisture is strongly affected by the surface moisture conditions, the polarization of the brightness temperature data, and the choice of the secondary ancillary parameter to be retrieved. The synthetic analysis demonstrated a tendency for better retrievals from dual-polarized data at large incidence angles (40-50°). Validation with airborne brightness temperature observations at L-band did not demonstrate such a strong angular dependency, although it confirmed that the simultaneous retrieval of soil moisture and vegetation properties is not preferable as opposed to i) soil moisture and surface roughness or ii) soil moisture and surface soil temperature, especially under dry moisture conditions.
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C03 01  X  FRE  @0 Sensibilité @5 01
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C03 02  X  FRE  @0 Paramètre @5 02
C03 02  X  ENG  @0 Parameter @5 02
C03 02  X  SPA  @0 Parámetro @5 02
C03 03  2  FRE  @0 Humidité sol @5 03
C03 03  2  ENG  @0 soil moisture @5 03
C03 03  2  SPA  @0 Humedad suelo @5 03
C03 04  2  FRE  @0 Angle incidence @5 04
C03 04  2  ENG  @0 incidence angle @5 04
C03 05  X  FRE  @0 Configuration @5 05
C03 05  X  ENG  @0 Configuration @5 05
C03 05  X  SPA  @0 Configuración @5 05
C03 06  X  FRE  @0 Bande L @5 06
C03 06  X  ENG  @0 L band @5 06
C03 06  X  SPA  @0 Banda L @5 06
C03 07  X  FRE  @0 Mesure angle @5 07
C03 07  X  ENG  @0 Angular measurement @5 07
C03 07  X  SPA  @0 Medida ángulo @5 07
C03 08  2  FRE  @0 Océan @5 08
C03 08  2  ENG  @0 ocean @5 08
C03 09  2  FRE  @0 Milieu marin @5 09
C03 09  2  ENG  @0 marine environment @5 09
C03 09  2  SPA  @0 Medio marino @5 09
C03 10  2  FRE  @0 Salinité @5 10
C03 10  2  ENG  @0 salinity @5 10
C03 10  2  SPA  @0 Salinidad @5 10
C03 11  2  FRE  @0 Algorithme @5 12
C03 11  2  ENG  @0 algorithms @5 12
C03 11  2  SPA  @0 Algoritmo @5 12
C03 12  2  FRE  @0 Végétation @5 13
C03 12  2  ENG  @0 vegetation @5 13
C03 12  2  SPA  @0 Vegetación @5 13
C03 13  2  FRE  @0 Teneur eau @5 14
C03 13  2  ENG  @0 water content @5 14
C03 13  2  SPA  @0 Contenido en agua @5 14
C03 14  2  FRE  @0 Rugosité @5 15
C03 14  2  ENG  @0 roughness @5 15
C03 14  2  SPA  @0 Rugosidad @5 15
C03 15  X  FRE  @0 Température sol @5 16
C03 15  X  ENG  @0 Soil temperature @5 16
C03 15  X  SPA  @0 Temperatura suelo @5 16
C03 16  2  FRE  @0 Modèle @5 17
C03 16  2  ENG  @0 models @5 17
C03 16  2  SPA  @0 Modelo @5 17
C03 17  X  FRE  @0 Modélisation @5 18
C03 17  X  ENG  @0 Modeling @5 18
C03 17  X  SPA  @0 Modelización @5 18
C03 18  2  FRE  @0 Température brillance @5 19
C03 18  2  ENG  @0 brightness temperature @5 19
C03 19  2  FRE  @0 Simulation @5 20
C03 19  2  ENG  @0 simulation @5 20
C03 19  2  SPA  @0 Simulación @5 20
C03 20  X  FRE  @0 Effet température @5 21
C03 20  X  ENG  @0 Temperature effect @5 21
C03 20  X  SPA  @0 Efecto temperatura @5 21
C03 21  X  FRE  @0 Etude sur terrain @5 23
C03 21  X  ENG  @0 Field study @5 23
C03 21  X  SPA  @0 Estudio en campo @5 23
C03 22  X  FRE  @0 Essai en champ @5 24
C03 22  X  ENG  @0 Field experiment @5 24
C03 22  X  SPA  @0 Ensayo en campo @5 24
C03 23  2  FRE  @0 Australie @2 NG @5 61
C03 23  2  ENG  @0 Australia @2 NG @5 61
C03 23  2  SPA  @0 Australia @2 NG @5 61
C07 01  2  FRE  @0 Australasie
C07 01  2  ENG  @0 Australasia
C07 01  2  SPA  @0 Australasia
N21       @1 167
N44 01      @1 OTO
N82       @1 OTO

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Pascal:14-0131784

Le document en format XML

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<s0>L band</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA">
<s0>Banda L</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="X" l="FRE">
<s0>Mesure angle</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="ENG">
<s0>Angular measurement</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="SPA">
<s0>Medida ángulo</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE">
<s0>Océan</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG">
<s0>ocean</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE">
<s0>Milieu marin</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG">
<s0>marine environment</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA">
<s0>Medio marino</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE">
<s0>Salinité</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG">
<s0>salinity</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA">
<s0>Salinidad</s0>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE">
<s0>Algorithme</s0>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG">
<s0>algorithms</s0>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA">
<s0>Algoritmo</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE">
<s0>Végétation</s0>
<s5>13</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG">
<s0>vegetation</s0>
<s5>13</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA">
<s0>Vegetación</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE">
<s0>Teneur eau</s0>
<s5>14</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG">
<s0>water content</s0>
<s5>14</s5>
</fC03>
<fC03 i1="13" i2="2" l="SPA">
<s0>Contenido en agua</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE">
<s0>Rugosité</s0>
<s5>15</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG">
<s0>roughness</s0>
<s5>15</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA">
<s0>Rugosidad</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="X" l="FRE">
<s0>Température sol</s0>
<s5>16</s5>
</fC03>
<fC03 i1="15" i2="X" l="ENG">
<s0>Soil temperature</s0>
<s5>16</s5>
</fC03>
<fC03 i1="15" i2="X" l="SPA">
<s0>Temperatura suelo</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE">
<s0>Modèle</s0>
<s5>17</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG">
<s0>models</s0>
<s5>17</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA">
<s0>Modelo</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="X" l="FRE">
<s0>Modélisation</s0>
<s5>18</s5>
</fC03>
<fC03 i1="17" i2="X" l="ENG">
<s0>Modeling</s0>
<s5>18</s5>
</fC03>
<fC03 i1="17" i2="X" l="SPA">
<s0>Modelización</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE">
<s0>Température brillance</s0>
<s5>19</s5>
</fC03>
<fC03 i1="18" i2="2" l="ENG">
<s0>brightness temperature</s0>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE">
<s0>Simulation</s0>
<s5>20</s5>
</fC03>
<fC03 i1="19" i2="2" l="ENG">
<s0>simulation</s0>
<s5>20</s5>
</fC03>
<fC03 i1="19" i2="2" l="SPA">
<s0>Simulación</s0>
<s5>20</s5>
</fC03>
<fC03 i1="20" i2="X" l="FRE">
<s0>Effet température</s0>
<s5>21</s5>
</fC03>
<fC03 i1="20" i2="X" l="ENG">
<s0>Temperature effect</s0>
<s5>21</s5>
</fC03>
<fC03 i1="20" i2="X" l="SPA">
<s0>Efecto temperatura</s0>
<s5>21</s5>
</fC03>
<fC03 i1="21" i2="X" l="FRE">
<s0>Etude sur terrain</s0>
<s5>23</s5>
</fC03>
<fC03 i1="21" i2="X" l="ENG">
<s0>Field study</s0>
<s5>23</s5>
</fC03>
<fC03 i1="21" i2="X" l="SPA">
<s0>Estudio en campo</s0>
<s5>23</s5>
</fC03>
<fC03 i1="22" i2="X" l="FRE">
<s0>Essai en champ</s0>
<s5>24</s5>
</fC03>
<fC03 i1="22" i2="X" l="ENG">
<s0>Field experiment</s0>
<s5>24</s5>
</fC03>
<fC03 i1="22" i2="X" l="SPA">
<s0>Ensayo en campo</s0>
<s5>24</s5>
</fC03>
<fC03 i1="23" i2="2" l="FRE">
<s0>Australie</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="23" i2="2" l="ENG">
<s0>Australia</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="23" i2="2" l="SPA">
<s0>Australia</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE">
<s0>Australasie</s0>
</fC07>
<fC07 i1="01" i2="2" l="ENG">
<s0>Australasia</s0>
</fC07>
<fC07 i1="01" i2="2" l="SPA">
<s0>Australasia</s0>
</fC07>
<fN21>
<s1>167</s1>
</fN21>
<fN44 i1="01">
<s1>OTO</s1>
</fN44>
<fN82>
<s1>OTO</s1>
</fN82>
</pA>
</standard>
</inist>
</record>

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