effects of fluvial morphology on remote sensing measurements of discharge american geophysical...
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![Page 1: Effects of Fluvial Morphology on Remote Sensing Measurements of Discharge American Geophysical Union, Fall Meeting, 2010 Session on “H66, The Remote Sensing](https://reader035.vdocuments.us/reader035/viewer/2022062407/56649d395503460f94a13360/html5/thumbnails/1.jpg)
Effects of Fluvial Morphology on Remote Sensing Measurements of
Discharge
American Geophysical Union, Fall Meeting, 2010Session on “H66, The Remote Sensing of Rivers”
G. R. BrakenridgeG. R. Brakenridge11, A.J. Kettner, A.J. Kettner11, I. Overeem, I. Overeem11, S.V. , S.V. NghiemNghiem22, T. De Groeve, T. De Groeve33, J.P. Syvitski, J.P. Syvitski11
11Dartmouth Flood Observatory and the CSDMS Facility, Dartmouth Flood Observatory and the CSDMS Facility, University of ColoradoUniversity of Colorado2 2 Jet Propulsion Laboratory , California Institute of TechnologyJet Propulsion Laboratory , California Institute of Technology33Joint Research Centre of the European CommissionJoint Research Centre of the European Commission
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Can Available Orbital Remote Sensing provide useful measurements of global
river discharge variability?
The Advanced Microwave Scanning Radiometer - Earth Observing System (AMSR-E) is a twelve-channel, six-frequency, passive-microwave radiometer. It measures horizontally and vertically polarized brightness temperatures, including at 36.5 GHz.
AMSR-E was developed by the Japan Aerospace Exploration Agency (JAXA) and launched by the U.S. aboard Aqua in mid-2002.
Monitoring of River Discharge Changes:A Passive Microwave Approach
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From USGS field dataFor this gauging station
From Smith et al, 1996, WRR.
Effective width = flow area/river length
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From Gage(4.5 ft rise)
To Discharge(via a rating curve)
There is a nearly 4x increase in discharge, over a periodOf 9 days.
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One day of AMSR-E data collection(high latitudes revisited most frequently)
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To measure surface water change:Traditional Method : Polarization Ratio
PR=(TbVTbH)/(TbV+TbH)
C
M
M is the Measurement cell containing the riverC is the Calibration cell with no river
New Method : Pair RatioHR=TbH(C)/TbH(M)VR=TbV(C)/TbV(M)
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Emission Model Analysis
Pair Ratio H-pol: HR=TbH(C)/TbH(M)Silt-loam soil:27% clay, 62% silt
Water fraction:fw=10-90%
Soil moisture %:Rain in M, not Cmv=10 M, 5 C (thin)mv=20 M, 5 C (bold)Rain in M and Cmv=10-35 (medium) in both M and C
36.5 GHz
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• Use H polarization at 36.5 GHz (6.92/10.65 RFI, 18.7/28.3 GHz water line,
89 GHz oxygen line)
• C is near M to be within correlation length scale of physical temperature T
• C and M are located to minimize differences in data acquisition time, and
over similar ground cover types.
• For calibration to be unaffected by river, C is chosen at location outside of
river reach M
• M is selected to conform with river reach to maximize surface water
change
• Use rating curve to calibrate HR (the paired ratio estimator) to stream flow
Protocol for River Flow Measurement
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Tb
dry
wet
Tb
dry
wet
Dry pixelWet pixel
Influence of other factors (clouds, ground temperature, etc) is much reduced by comparing dry and wet signal
Water has a lower brightness
temperature than land
1
2
3
1 2 31 2 3
flood signal
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Example: Wabash River near Mount Carmel, Illinois, USA
Black square showsMeasurement pixel(blue line in next plot)
White square iscalibration pixel(green line in next plot)
Dark blue colors:Flooding mapped byMODIS
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Scatter Plot of AMSR-E HR ratio (calibration site/measurement site) versusWabash River discharge. Plot is uncorrected for any lag times .
As discharge rises above bankful state, HR increased from 1.05 to 1.1.
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Wabash River in U.S.Near New Harmony, Indiana
Brown = estimated discharge from AMSR-E dataBlack= USGS in-situ stream gauge data
Green = brightness temperature of calibration siteBlue= brightness temperature of river measurement site.
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Portion of the estimated discharge time series (black) compared to local gauging station discharge (blue line).
Satellite-estimated discharge lags gauging station discharge..
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Estimated discharge time series (black) compared to local gauging station discharge (blue line), with a lag applied.
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No time lag.
With time lag.
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Flood in March 2006 along the Wabash River recorded by the gauging station (lower plot, bold black line) and by HR from AMSR-E data (lower plot, thin black line).
Due to inundation dynamics, peak discharge was reached at the gauging station 2–3 days before peak discharge as inferred from the AMSRE. From Brakenridge et al (2007) WRR.
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River Watch Site496, White River near Augusta.
Channel is 170 m in width, with sinuous meanders.
Circle is area of river measurement reach.
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Green line is upwelling microwave radiance within 5 km radius of a calibration land targetBlue line is radiance within 5 km radius of a river measurement site targetBrown line is their ratio and is used to estimate discharge via a rating equation.
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Preliminary rating curve for this site.
This equation used to estimate discharge, using remote sensing data (in black, above)
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Monthly Runoff, calculated from daily mean discharge, ground station
Monthly Runoff, calculated from AMSR-E data
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Annual Runoff
(mm)
60
274
298
351
169
367
549
608
482
Annual Runoff
(mm)
118
307
299
365
151
384
702
633
440
Yearly Runoff, calculated from daily mean gauging station discharge
Yearly Runoff, calculated from AMSR-E data
200220032004200520062007200820092010
200220032004200520062007200820092010
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Measured rainfall (blue), modeled river Q (green), gauged Q (red) and AMSR-E Q (orange) for the Okavango R, Botswana. AMSR-E calibrated to discharge by a simple linear equation. An improved rating equation would correct the over-estimation of low flow
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Can Available Orbital Remote Sensing provide useful measurements of global
river discharge variability?
Constraints
1.Data are less precise than in-situ gauging.2.Conversion of the estimator to actual discharge requires ground-based data.
Benefits
1.The signal alone, without any calibration to discharge, still allows prompt characterization of anomalies (floods and droughts).2.Adequate calibration to actual discharge has been obtained at many sites via comparison of monthly mean, maximum and minimum values: so, existing global runoff data can be used, now, to calibrate a global array of sites.3.There is clear potential for an accurate global river measurement system that can be updated in real time, and, via SSMI microwave data, extended back into the 1980s.
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Location of river gauging stations on the grounds, with various data archived at the Global Runoff Data Centre. Periods of record, type of information varies widely. Many usage restrictions apply. Very little real time data are available on international basis.
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Location of presently measured sites using AMSR-E data. Data can be updated daily; are consistent through time, extend back to mid-2002, could be extended to mid 1980s using DMSP/SSMI 36 GHz data.
NASA’s GPM will provide abundant new data forward in time.
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Why not use what is available, from ground based data, in order to calibrate, produce rating curves, for satellite-based river measurement sites? This is optimum use of available data.
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October 12, 2010
River Watch Measurement Sites
Red: Purple: Blue: Yellow:
Major flooding, > 5yr recurrenceModerate flooding, >1.3 yr recurrenceNormal flowLow flow or ice-covered
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November 7, 2010
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November 17, 2010
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December 8, 2010