jet propulsion laboratory topography (swot) mission · from l2 pixel cloud. options: – nasa/cnes...
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National Aeronautics and Space Administration Jet Propulsion Laboratory California Institute of Technology Pasadena, California
Surface Water and Ocean Topography (SWOT) Mission
River Data Products and Func2onal Flow Michael Durand
Ohio State University
Sylvain Biancamaria LEGOS
14 January 2015
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Status
• Discussed in some depth at the first Algorithm Definition Team meeting in New York (October 2014)
• What is being defined is not the L2 point cloud, but (largely) vector products derived therefrom
• Based on these discussions, produced a 10-page proposal / draft description of products, which was circulated to the ADT
• This draft was discussed via telecon
• Goal today is to solicit feedback from the SDT on proposed river products
• Product definitions are currently flexible and can be discussed!
• Future version of the simulator will include many of these attributes as part of the River Vectorizer
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Guiding Philosophy
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Rivers & Co. ~ A taxonomy
1. Rivers
1. Single-channel planforms
2. Simple multi-channel planforms
3. Braided and anastamosing planforms
4. Floodplain-river systems
2. Reservoirs
3. Spillways, dams and waterfalls
4. Tidal reaches
5. Low spatial resolution product Case 1.1 will represent many rivers. Special cases are more challenging.
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Products for single-channel planform
1. Polygon product showing river inundated area 2. Centerline products 3. Attributes of the center-line/polygon products
1. Reach ID 2. River name 3. Reach length 4. Reach-averaged height & uncertainty 5. Reach-averaged slope & uncertainty 6. Reach-averaged inundated area & uncertainty 7. Reach-averaged discharge & uncertainty 8. Time-invariant parameters used in discharge calculation
Descrip8on currently applies to pass-‐based products, only. Cycle-‐based or monthly products are currently being discussed
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Products for single-channel planform
3. Attributes of the center-line/polygon products (cont.) 9. Island detection flag 10. River planform classification 11. Quality and other flags (ice/snow/high precipitation rate, etc.) 12. Connectivity: upstream and downstream reaches
Descrip8on currently applies to pass-‐based products, only. Cycle-‐based or monthly products are currently being discussed
A revision to this has been proposed by Ernesto et al. in which products would be evaluated at nodes con8nuous along the river centerline. The first draB of the “river vectorizer” has been released to the ADT and includes addi8onal products such as minimum & maximum longitude & la8tude, pass number, etc.
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Example courtesy Ernesto
1. Reach ID: 3 2. River Name: Ohio 3. Reach length: 8391.3 m 4. Height: 161.67 m 5. Slope: 14.73 cm/km 6. Area: 1568429.9 m2
7. etc.
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Rivers & Co. ~ A taxonomy
1. Rivers
1. Single-channel planforms
2. Simple multi-channel planforms
3. Braided and anastamosing planforms
4. Floodplain-river systems
2. Reservoirs
3. Spillways, dams and waterfalls
4. Tidal reaches
5. Low spatial resolution product
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Case 1.2: Simple multi-channel planforms
• Where possible, multiple channels will be considered separate objects, with their own attributes
• Where not possible, their inundated area will be merged, average height calculated, and “multiple-channel” flag set
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50
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650 660 670 680 690 700
Chan
nel w
idth [m
] River flow distance [km]
Channel 1 (Main) Channel 2 Channel 3
Seine River model: courtesy Nicolas Flipo
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Case 1.3: Braided and Anastamosing planforms
• Where possible, individual channels will have separate products. A nomenclature for reach connectivity will be developed
• Where multiple channels cannot be resolved, aggregate products will have to be developed, starting with the RivWidth-style approach
• To be explored using instrument simulator runs
Tanana River model, courtesy Elizabeth Humphries, UNC
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Case 1.4: River-Floodplain systems
• In the floodplain for 2-D flow, 2-D gridded products are needed: rasters from L2 pixel cloud. Options: – NASA/CNES pre-stages products over select areas – NASA/CNES provides online web tools where users select areas and
products are served up – Tools are provided so users can resample the pixel cloud as they wish
Logone River floodplain, Cameroon Amazon floodplain. Alsdorf et al., 2007
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Case 2: Reservoirs
• Reservoirs will be treated as lakes in terms of their products. Will be included in the river databases for along-stream continuity
• Will use a priori databases of reservoir locations. This will be refined using the first year of SWOT data
Priest Rapids Lake, along the Columbia River
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Case 3: Spillways, dams, and waterfalls
• In some cases, drops occur over very short distances. Usual products cannot be calculated
• Instead, an “elevation drop” product will be calculated • Similar to case 2, an a priori database will be refined after
one year of SWOT data
Newburg Lock and Dam on the Ohio River. Eleva8ons via the Community HEC-‐RAS model.
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Case 3: Spillways, dams, and waterfalls
• In some cases, despite drops occurring over short distances, the drops are small (decimeter) and distance between drops is small (e.g. <10 km).
• In these cases, average height and slope will be calculated
In situ GPS measurements along the Olentangy River. Summer, 2014.
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Case 4: Tidal Reaches
• Nominally we will produce the same products used for case 1.1
• Need to determine where each river ends. How will this be determined?
• Many of these reaches will be very low slope: At what point do we say slope cannot be accurately produced? E.g. would we really want to say slope is 0.1 cm/km ± 1 cm/km?
• These need to be assessed in the context of instrument simulation of tidal reaches
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Case 5: Low-resolution product
• It’s not clear in what cases this product would have value (under investigation by the ADT)
• The product might have value over floodplains with significant inundation extent, or over large reservoirs in line with the river network
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The polygon product
• Due to classification and geolocation issues, it is not clear that a reliable 2-D polygon mask can be produced
• Science requirements stress total inundated area, which can be produced
• Current philosophy:
– If we can produce the polygon reliably, then we should do so
– If we cannot, we should re-evaluate whether to produce
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Floods
• What data product should be produced for floods?
• Perhaps we could produce a gridded product similar to the floodplain product, when that is defined?
Water depth. Simula2on courtesy Jeremiah Lant.
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Dra= of River Processor flow chart for single-‐channel planform rivers. FuncEonal flow will be refined a=er data products are beHer specified.
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River Simulation Priorities
• Sacramento River: 100 m wide. In progress. • Upstream Garonne: 100 m wide. Complete. • Platte River: 50-100 m wide. Braided. Complex
dynamics. Complete. • Tanana: 400-600 m wide. Braided. Complex dynamics. • St Lawrence: Includes lakes, multiple channels. • Seine Estuary: Tidal area. Includes some 2-D flow. In
progress. • Connecticut: Tidal, relatively wider. Some floodplain
interaction. • Downstream Garonne: Less steep and wider than
upstream reach. Almost complete.
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Summary
• Initial product definitions taxonomy, and product differentiation has been proposed
• New river products from Ernesto are excellent. The upcoming new version the simulator that includes these is critical
• Decisions on polygons, products in complex environments are upcoming
• Need to determine who is going to define estuarine data products
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Questions for Discussion
• Is the hierarchy correct?
• What difficult and special cases are missing?
• What are the right priorities for simulation and further study?
• What other data products should be produced?
• What products should be produced in complex environments?
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Extra Slides
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Basic Func2onal Flow Details
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Snap water pixels to reaches
• Inputs: – SWOT pixel cloud
• classification • height • associated accuracy
– Static database of reach boundaries • Defined a priori • Perhaps refined after a period of SWOT data available
• Purpose: – Determine which pixels are associated with which reaches – Currently we will assume a one-to-one mapping (in theory,
the same pixel could be used to inform reach-properties of multiple reaches)
• Output: – A database linking pixels on each pass to reaches
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Centerline calculation & multi-channel handling
• Inputs: – SWOT pixel cloud & map to reaches – Static database of reach boundaries
• Purpose: – Determine river centerline (needed for slope calculations), which
can be dynamic from pass-to-pass – Determine flow distance along centerline – For now, assume the RivWidth approach to centerline calculation
for braided rivres • Output (on a per pass basis)
– River centerline – Reach length
• Issues – What do the products look like for massively braided rivers?
Need example instrument simulator runs for these cases
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Centerline reach-averaged height & slope
• Inputs – River centerline and flow length along the centerline for
each reach – SWOT pixel cloud and map to each reach
• Purpose – For 1D rivers: Snap pixels to centerline to associate them
with a 1-D flow distance (less trivial than it sounds) – Reach average slope should be in the 1-D direction.
Heritage: fit first-order polynomial to each reach – Reach average height should be straightforward.
• Issues – How to handle 2-D flow environments? – How to handle lakes along river network? – How is uncertainty calculated?
• Output: reach average height, slope, and uncertainty
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Inundated extent and reach average width
• Inputs – SWOT pixel cloud and map to each reach – Flow distance for each reach
• Purpose – Calculate total inundated extent: probabilistic algorithm
being explored – Reach average width would be inundated extent divided by
reach length • Issues
– How to handle 2-D flow environments? – How to handle lakes along river network? – How is uncertainty calculated? – Is a polygon being considered?
• Output: inundated extent, reach average width
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Inversion of hydraulic parameters for discharge calculation
• Inputs – Reach average height, width, and slope – Prior first guess of reach average hydraulic parameters
(e.g. bathymetry & roughness coefficient) • Purpose
– Calculate optimal hydraulic parameters for each reach, probably after receiving several seasons or one year of SWOT data
– This would be done as a one-time or special-case step: not iteratively with each new pass or cycle
• Issues – How to handle 2-D flow environments? – How to handle lakes along river network?
• Output: database of hydraulic parameters
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Operational discharge production
• Inputs – Reach average height, width, and slope – Optimal hydraulic parameters
• Purpose – Calculate discharge on a per-pass basis, probably using
Manning’s equation • Issues
– How to handle 2-D flow environments? – How to handle lakes along river network? – Should we apply some operational flow constraints to
ensure continuity? • Output: database of reach-averaged river discharge