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Snow Hydrology: Microwave Interaction with Snowpack Do-Hyuk “DK” Kang Environmental Engineering University of Northern British Columbia December 5 th, 2013 Northern Hydrometeorology Group
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Frolov and Marchert 1999, Hallikainen et al. 1986, TGRS
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EM WAVE PROPAGATION TX RX TX Inan and Inan Electromagnetic Waves,
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Hallikainen et al. 1986, TGRS
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RF SYSTEM DESIGN TRANSMITTER: BY VADUM INC RECEIVER: NI VSA & PREAMP
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LABORATORY TEST
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Amplitudes and Histograms
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Phase and Fourier Transforms
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Key Words Matzler and Wiesmann 1999 Devonec and Barros 2002 TbTb TsTs p ec freq LWC
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Model Setup State Variables (SWE [m], Snow depth [m], Snow density [kg/m 3 ], Snow Temperature [K], and Grain Size (will be) at each layer from 1st to nth layer 1-D Column simulation both for snow physics and radiation schemes with multi-layer Hourly Met. Data needed to drive model Output: Hourly Vertical Profiles of Snowpacks, Corresponding Tb [K], emissivity [ ], and Teff [K]
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Site Descriptions Valdai, Russia, 78~83, SMMR, 25X25 km CLPX 2002-2003, 02~03, SSM/I, AMSR-E 25X25 km
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Coupled Model I : Snow Physics Mass Balance Energy Balance
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Coupled Model II : Snow Radiation Kang and Barros 2010 Matzler and Wiesmann 1999
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VALDAI
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CLPX
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Schanda and Matzler 1981 Willis et al. 2012 RS and Env Kang et al. 2012 Accepted in IEEE
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Kang et al. 2012 Accepted in IEEE
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Kang et al. 2012 Accepted in IEEE
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Wiscomb and Warren 1980 VS Mätzler 2000 2997924 GHz = infrared 37 GHz = microwave
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Ice-Lamellae Model (Mätzler 2000, DK imp.) Six flux theory: r, t, and e
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Scattering: multi freq.
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Future Topics Grain size Ice lenses within snow layers Depth hoar/surface hoar First snow Intensity (radiative trnaser) Electric Dipole Moment Impedance Matching
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Questions
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Schanda and Matzler 1981 Willis et al. 2012 RS and Env Kang et al. 2012 Accepted in IEEE
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Kang et al. 2012 Accepted in IEEE
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Kang et al. 2012 Accepted in IEEE
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Dry Snow VS Wet Snow
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Dry Snow Wet Snow
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Water Presence
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Coupled Model Kang and Barros 2010 Matzler and Wiesmann 1999
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Matzler and Wisemann 1999 RS and Env
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BC ministry, Environment Canada
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VIC application to FRB
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Summary Introduced L band Snow Sensor Simulated Snow Physics and Radiation Physics in both Valdai and CLPX 2002 Future View NCEP based model application into FRB NARR based model application into FRB expected Paper 1: point scale snow hydrology assessment + VIC watershed scale investigation Radar response Paper 2: grain size, LWC toward radar backscattering signals
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Key Words Matzler and Wiesmann 1999 Devonec and Barros 2002 pol. p ec freq Water incluson
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Hallikainen et al. 1986, TGRS Colbeck 1974
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Based on Chang et al. 1987
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CLPX
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VALDAI
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CLPX
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Outline Coupled multi-layered snow physics model with passive microwave simulator Demonstrated model performance at two different locations:1) Valdai, Russia and 2) CLPX 2002
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Model Setup State Variables (SWE [m], Snow depth [m], Snow density [kg/m3], Snow Temperature [K], and Grain Size (will be) at each layer from 1st to nth layer 1-D Column simulation both for snow physics and radiation schemes Hourly Met. Data from RUC40 MM5 Output: Hourly Vertical Profiles of Snowpacks, Corresponding Tb, es, and Teff [K]
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VALDAI
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Dry Snow VS Wet Snow
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Coupled Model II : Snow Radiation Kang and Barros 2010 Matzler and Wiesmann 1999
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dry Snow case
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Wet Snow case
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Part 1: Motivations History of Snow Hydrology Model Legacy of Microwave Remote Sensing of Snowpack Challenge in measurement of snowpack Snow Hydrology Forward Radiation Coupled Model
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Hallikainen et al. 1986, TGRS Colbeck 1974
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Key Words Matzler and Wiesmann 1999 Devonec and Barros 2002 TbTb TsTs
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Part 2: Implementation Snow Physics Model Snow Radiation Model Challenge in measurement of snowpack Physics Model Radiation Model Coupled Model
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Key Words Radiation Physics Matzler and Wiesmann 1999 Devonec and Barros 2002
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http://www.ipac.caltech.edu/outreach/Edu/Windows/irwindows.html
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Hallikainen 1986, TGRS
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