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Applying Longterm SSMI Observations to Dust Storm Study

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Explore the potential role of microwave remote sensing in dust storm monitoring ... channel, four-frequency (19.35, 22.235, 37, and 85.5 GHz) microwave radiometer ... – PowerPoint PPT presentation

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Title: Applying Longterm SSMI Observations to Dust Storm Study


1
Applying Long-term SSM/I Observations to Dust
Storm Study
  • Jinyang Du
  • USDA-ARS Hydrology Remote Sensing Lab
  • Aug 27-29, 2007, Boulder

2
Objectives
  • Explore the potential role of microwave remote
    sensing in dust storm monitoring
  • Use long-term microwave satellite observations to
    study the change of earth surface conditions
  • Demonstrate the relationship between Microwave
    Indexes and ground surface parameters of dust
    storm source regions
  • Scattering Index
  • Polarization Index
  • Impact of current and future microwave satellites
    on dust storm monitoring

3
Special Sensor Microwave Imager (SSM/I)
  • Seven-channel, four-frequency (19.35, 22.235, 37,
    and 85.5 GHz) microwave radiometer
  • conically scanning
  • Incidence angle 53 degree
  • Data from SSM/I mounted on Defense
    Meteorological Satellite Program (DMSP) F13
    platform are used in the study
  • (Data source NSIDC)

4
Study Region- Ordos Plateau of China
  • 3720'4050'
  • 10624'11128'
  • A transitional zone of arid to semi-arid climates
  • One of the Asian dust-storm source regions

5
Scattering Index
  • Precipitation and Snow are masked out
  • Scattering Index can be used to evaluate feature
    scattering properties
  • Dry loose soil particles can be strong scatterers

SI451.88-0.44Tb_19v-1.775Tb_22v0.00574Tb_22v
Tb_22v Tb_85v (Ferraro et al.,
1994)
6
Polarization Index
Global Polarization Index Map
Global NDVI Map
PI(Tb_v-Tb_h)/(Tb_vTb_h)
7
Scattering Index (April, Erdos Plateau)
Compare SI and Number of dust-storm days observed
from meteorology station
8
Polarization Index (May, Erdos Plateau)
Compare PI and Number of dust-storm days observed
from meteorology station
9
Summary
  • Microwave remote sensing can provide unique
    ground surface information
  • SI and PI derived from SSM/I observations can be
    used to monitor the surface condition of sand
    storm regions
  • Long-term earth observations from current
    microwave satellites SSM/I, AMSR-E, WindSat and
    future L-Band satellites (SMAP, SMOS) will help
    to understand the change of land surface
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