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Analysis of the passive microwave high-frequency signal in the shallow snow retrieval 2011 IEEE Geoscience and Remote Sensing symposium Jul. 24-29, Vancouver, Canada [email_address]   28 th  Jul. 2011 AMSR-E Y.B. Qiu 1*,  H.D. Guo 1 , J.C. Shi 2 , S.C. Kang 3 J. Lemmetyinen 4 , J.R. Wang 5 1 Center of Earth Observation and Digital Earth, CAS, China 2 University of California, Santa Barbara, USA 3 Institute of Tibetan Plateau Research, CAS, China 4 FMI, Arctic Research Centre, Finland 5 NASA Goddard Space Flight Center, Greenbelt, USA
Outline ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Snow - a potentially sensitive factor of climate change ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Nine GCM model: shrinking snow cover over Northern American   ( Frei, A. and G. Gong, 2005.  ) Why Snow?
Will Climate Change Affect Snow Cover Over North America?   ,[object Object],[object Object],Why Snow?  debate New debate ?
Snow Cover Distribution, Variability, and Response to Climate Change in Western China ,[object Object],[object Object],Potential impact of climate change on snow cover area in the  Tarim River  basin QIN DAHE, 2006 Xu Changchun, 2007 ,[object Object],[object Object],[object Object],China – Publication’s View
Western China Tibet Plateau Northern China Xinjiang Mongolia Northeast The select test areas in China ,[object Object],[object Object],[object Object],[object Object],Part I: Analysis in China from the nowadays products: Qinghai Xinjiang Tibet Qinghai Tibet
Western China Area Tibet Plateau Northern China Agree well with the previous publication , but the snow cover area over Tibet is  not quite right . Rutger snow product 1966.11~2010.5
China – decreasing SCA/SWE over Tibet Plateau SMM/I SWE product Tibet Plateau Tibet Plateau 1978-2007
NOAA IMS   1997-2010 SCA Tibet Plateau Western China decreasing decreasing
NOAA IMS   1997-2010 SCA Northern China The NOAA IMS show different Trend with above two publications and the Rutger’s result. Increasing ,[object Object],[object Object],[object Object],[object Object],[object Object]
We get: ,[object Object],[object Object],[object Object],Need More accurate snow data
Part II: Passive Microwave remote sensing of snow ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],For dry snow
Passive Microwave remote sensing of snow ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],TB(37-19V) (K) Station Snow Depth (cm)
Shallow snow situation in China – western China, especially the Tibet area Menyuan station Maduo station ,[object Object],[object Object],Sparse Station
Shallow snow situation in China – western China 52985 Hezheng, Gansu (35.42N, 103.33E)   Snow depth < 10cm 56093 Minxian, Gansu (34.43N, 104.02E)
Part III:   Possibility analysis of the high frequencies in the shallow snow retrieval HUT snow model simulation 36GHZ/18.7GHz gradient Shallow snow sensitive 89GHZ-18.7GHz gradient Shallow snow sensitive
Comparison: In-situ snow depth and SMMR, SMM/I, and AMSR-E emission signal ,[object Object],[object Object],[object Object],[object Object],Comparison of the traditional algorithm records and Snow depth ,[object Object],[object Object]
Tree-free, sparse vegetation area, taken at the winter of 2010  Less than 20cm NamCo station
Snow depth (cm) from NamCo station and AMSR-E TBs Compare with the NASA algorithm SWE result TB(35GHz-18.7GHz) TB(89GHz-18.7GHz) Snow depth (cm) SWE (mm)/NASA ITPR,CAS
Snow depth (cm) and AMSR-E TBs (2009~2010) 50727 (47.17N 119.93E) Heilongjiang   50434 50.48N 121.68 E Neimenggu
Snow depth (cm) and AMSR-E TBs (2009~2010) 54049 44.25N 123.97E Jilin   52681 38.63N 103.08E Gansu
Snow depth (cm) and AMSR-E TBs (2009~2010) 53231 41.40N 106.40E Neimenggu   53519 39.22N 106.77E Ningxia   89GHz is sensitive to the snow occurrence (fresh snow flake)
Snow depth (cm) and SSM/I TB Gradient ,[object Object],[object Object],[object Object],[object Object]
Snow depth and SSM/I TB Gradient 36665 ZAJSAN   36870 ALMA-ATA   TB(37-19GHz) and TB(85-19GHz) ‘s response to the snow evolution
38618 FERGANA   38599 LENINABAD   High frequency shows a sensitive response to the shallow snow  Snow depth and SSM/I TB Gradient
Snow depth and SSM/I TB SAMARKAND 38696   KURGAN-TJUBE 38933   High frequency shows a sensitive response to the shallow snow
Possible algorithm development with high frequencies and analysis We apply the ATC Chang(1987) gradient algorithm SD = a* (Tb18H - Tb37H) + b Firstly, we exam the relatively deep snow over rich forest area.
1987-1991  snow depth and SMM/I Tbs,  261 samples R-square: 0.71428 a=-6.98161 b= -0.35971 Possible algorithm development with high frequencies and analysis
1987-1991  snow depth and SMM/I Tbs,  261 samples R-square: 0.05764 a=-18.95129 b= -0.12906 R-square: 0.2509 a= -11.96944 b= 0.23074 Grain Size =1.3~1.7mm Possible algorithm development with high frequencies and analysis
1992-1995  snow depth and SMM/I Tbs,  640 samples R-square: 0.48892 a= -6.24384 b= -0.26904 Possible algorithm development with high frequencies and analysis
1992-1995  snow depth and SMM/I Tbs,  640 samples R-square: 0.00456 a= -17.45683 b= -0.03825 R-square: 0.33649 a= -11.21299 b= 0.23079 Thick snow Thick snow Possible algorithm development with high frequencies and analysis
1988-1995  snow depth and SMM/I Tbs,  420 samples R-square:0.31795 a= -6.66873 b=-1.07606 Shallow snow Possible algorithm development with high frequencies and analysis R-square:0.36473 a=-19.22 b=-1.5358
Select area –Tibet Plateau Possible algorithm development with high frequencies and analysis
1987-1995  snow depth and SMM/I Tbs,  469 samples Possible algorithm development with high frequencies and analysis
1987-1995  snow depth and SMM/I Tbs,  1353 samples The pair 85.0/19 shows its shallow snow retrieval ability and when the snow depth over 20cm, the signal is more variable and suspect. Possible algorithm development with high frequencies and analysis
Atmosphere influence issue ,[object Object],Ground Satellite Tb(36.5GHz-18.7GHz)
Atmosphere influence analysis ,[object Object],89.0GHz-18.7GHz Satellite Ground Atmosphere influence
Conclusion ,[object Object],[object Object],[object Object],[object Object],[object Object]
Thank you very much!

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TH4.TO4.5.ppt

  • 1. Analysis of the passive microwave high-frequency signal in the shallow snow retrieval 2011 IEEE Geoscience and Remote Sensing symposium Jul. 24-29, Vancouver, Canada [email_address] 28 th Jul. 2011 AMSR-E Y.B. Qiu 1*, H.D. Guo 1 , J.C. Shi 2 , S.C. Kang 3 J. Lemmetyinen 4 , J.R. Wang 5 1 Center of Earth Observation and Digital Earth, CAS, China 2 University of California, Santa Barbara, USA 3 Institute of Tibetan Plateau Research, CAS, China 4 FMI, Arctic Research Centre, Finland 5 NASA Goddard Space Flight Center, Greenbelt, USA
  • 2.
  • 3.
  • 4.
  • 5.
  • 6.
  • 7. Western China Area Tibet Plateau Northern China Agree well with the previous publication , but the snow cover area over Tibet is not quite right . Rutger snow product 1966.11~2010.5
  • 8. China – decreasing SCA/SWE over Tibet Plateau SMM/I SWE product Tibet Plateau Tibet Plateau 1978-2007
  • 9. NOAA IMS 1997-2010 SCA Tibet Plateau Western China decreasing decreasing
  • 10.
  • 11.
  • 12.
  • 13.
  • 14.
  • 15. Shallow snow situation in China – western China 52985 Hezheng, Gansu (35.42N, 103.33E) Snow depth < 10cm 56093 Minxian, Gansu (34.43N, 104.02E)
  • 16. Part III: Possibility analysis of the high frequencies in the shallow snow retrieval HUT snow model simulation 36GHZ/18.7GHz gradient Shallow snow sensitive 89GHZ-18.7GHz gradient Shallow snow sensitive
  • 17.
  • 18. Tree-free, sparse vegetation area, taken at the winter of 2010 Less than 20cm NamCo station
  • 19. Snow depth (cm) from NamCo station and AMSR-E TBs Compare with the NASA algorithm SWE result TB(35GHz-18.7GHz) TB(89GHz-18.7GHz) Snow depth (cm) SWE (mm)/NASA ITPR,CAS
  • 20. Snow depth (cm) and AMSR-E TBs (2009~2010) 50727 (47.17N 119.93E) Heilongjiang 50434 50.48N 121.68 E Neimenggu
  • 21. Snow depth (cm) and AMSR-E TBs (2009~2010) 54049 44.25N 123.97E Jilin 52681 38.63N 103.08E Gansu
  • 22. Snow depth (cm) and AMSR-E TBs (2009~2010) 53231 41.40N 106.40E Neimenggu 53519 39.22N 106.77E Ningxia 89GHz is sensitive to the snow occurrence (fresh snow flake)
  • 23.
  • 24. Snow depth and SSM/I TB Gradient 36665 ZAJSAN 36870 ALMA-ATA TB(37-19GHz) and TB(85-19GHz) ‘s response to the snow evolution
  • 25. 38618 FERGANA 38599 LENINABAD High frequency shows a sensitive response to the shallow snow Snow depth and SSM/I TB Gradient
  • 26. Snow depth and SSM/I TB SAMARKAND 38696 KURGAN-TJUBE 38933 High frequency shows a sensitive response to the shallow snow
  • 27. Possible algorithm development with high frequencies and analysis We apply the ATC Chang(1987) gradient algorithm SD = a* (Tb18H - Tb37H) + b Firstly, we exam the relatively deep snow over rich forest area.
  • 28. 1987-1991 snow depth and SMM/I Tbs, 261 samples R-square: 0.71428 a=-6.98161 b= -0.35971 Possible algorithm development with high frequencies and analysis
  • 29. 1987-1991 snow depth and SMM/I Tbs, 261 samples R-square: 0.05764 a=-18.95129 b= -0.12906 R-square: 0.2509 a= -11.96944 b= 0.23074 Grain Size =1.3~1.7mm Possible algorithm development with high frequencies and analysis
  • 30. 1992-1995 snow depth and SMM/I Tbs, 640 samples R-square: 0.48892 a= -6.24384 b= -0.26904 Possible algorithm development with high frequencies and analysis
  • 31. 1992-1995 snow depth and SMM/I Tbs, 640 samples R-square: 0.00456 a= -17.45683 b= -0.03825 R-square: 0.33649 a= -11.21299 b= 0.23079 Thick snow Thick snow Possible algorithm development with high frequencies and analysis
  • 32. 1988-1995 snow depth and SMM/I Tbs, 420 samples R-square:0.31795 a= -6.66873 b=-1.07606 Shallow snow Possible algorithm development with high frequencies and analysis R-square:0.36473 a=-19.22 b=-1.5358
  • 33. Select area –Tibet Plateau Possible algorithm development with high frequencies and analysis
  • 34. 1987-1995 snow depth and SMM/I Tbs, 469 samples Possible algorithm development with high frequencies and analysis
  • 35. 1987-1995 snow depth and SMM/I Tbs, 1353 samples The pair 85.0/19 shows its shallow snow retrieval ability and when the snow depth over 20cm, the signal is more variable and suspect. Possible algorithm development with high frequencies and analysis
  • 36.
  • 37.
  • 38.
  • 39. Thank you very much!