WaTER/Hydrosphere Mapper :

A wide swath altimetry mission for hydrology and oceanography

Lee-Lueng FuDouglas Alsdor fNelly Mognard

OSTST Meeting, March 12-15, 2007Hobar t, Australia

• At the Venice meeting a year ago, Hydrosphere Mapper and WaTER were separately presented as potential future missions using wide-swath altimetry technique.

• Via a workshop held in last October , the oceanography and land hydrology communities discussed their respective requirements and found that a single mission was able to meet the needs of both communities (http://ear thsciences.osu.edu/~alsdor f/files/WideSwath/)

• A joint oceanography and hydrology session was held in last AGU, showing the wide range of science and application oppor tunities provided by a joint WatER/Hydrosphere Mission.

• Such a mission has been recommended as Sur face Water and Ocean Topography (SWOT) mission by the NRC Decadal Survey for launch in the time frame of 2013-2016.

Progress made since the Venice Meeting

Small-scale Var iability of the Ocean Unresolved by Nadir -looking Altimeter

100 km

ground tracks of Jason (thick) and T/P (thin) Tandem Mission

100 km scale eddies resolvable by WSOA

10 km scale eddiesResolvable by HM

41.9º N

42.5º N

< 10 km

< 10 km

Coastal currents have scales less than 10 km

< 10 km

Observations made by ADCP offshore from the US

West CoastT. Strub

δδδδ h ~ 5 cmδδδδ v ~ 50 cm/sec

Scott (2005)

McWilliams (2006)

Sub-mesoscalevar iability

Sub-mesoscaleprocesses are poor ly observed but impor tant to the understanding of the dissipation mechanism of ocean circulation.

Radius of deformation

Radius of deformation

Altimetry SSH wavenumber spectrum

Wavenumber (cycles/km)

Pow

er d

ensi

ty (

cm2 /

cycl

es/k

m)

Noise level of WaTER/HM for 2 cm measurement noise at 2 km resolution

Jason pass 132 (147 cycle average)

Much reduced noise floor will enable the study of the spectrum at sub-mesoscaleswhich have not been well resolved from existing data.

Measurements Required to Address Science & Applications Themes: h, ∂h/∂x, ∂h/∂t, and area,

globally, on a ~weekly basis

�S = Σ ∂h/∂tPhotos: B. Kiel, K. Frey

Siberian Arctic

Muskingum R., Ohio

∂q – Q∂ x = ∂h

∂tL

∂h( )Q =

A ∂xRn

2/31/2

Continuity Equation

A Typical Flow Law

A = cross sectional areaR = wetted perimeterBoth can be mapped over time with repeated h measurements

Amazonian wetlands are 750,000 km2

Alaskan braided river

K. Douce Photo

Problems with 1D Stream Gauge Measurements

USGS Coverage: ~7000 gauges

Gauging from Space � WaTER/HM

Birkett, C.M., L.A.K. Mertes, T. Dunne, M.H. Costa, and M.J. Jasinski,Journal of Geophysical Research, 107, 2003.Hirsch, R.M., and J.E. Costa, EOS Transactions AGU, 85, 197-203, 2004.

Amazon: 6 M km2, ~175,000 m3/sU.S.: 7.9 M km2, Mississippi ~17,500 m3/s

OSTP 2004:“ Does the United States have enough water? We do not know.”“ What should we do? Use modern science and technology to determine how much water is currently available …”

�Using a radar altimeter, 32% of the rivers and 72% of the world’s lakes are not sampled

Topex/POSEIDON: ~70 points

Targets are Global

Matthews, E. and I. Fung, GBC, 1, 61-86, 1987.

Peace-Athabasca Delta: 3200 km2

Coastal Zones

Braided Rivers Reservoirs Worldwide

Floods

Congo River Basin: 3.7M km2

New Orleans

Ohio R.

Costa Rica

Canada

AlaskaN. Korea

WaTER/Hydrosphere MapperA SAR inter ferometry radar altimeter Near-global coverage with

16-day repeat orbit

• Same technique as WSOA – radar inter ferometry• Use of SAR to enhance the along-track resolution• 2 cm measurement precision at 2 km resolution• 1 micro-radian precision in mean sea sur face slope at 2 km resolution • No data gap near the coast

87654321 N

umbe

r of

Obs

erva

tion

Tidal aliasing of sun-synchronous orbit

0.0

200.0

400.0

600.0

800.0

1000.0

1200.0

1400.0

0 5 10 15 20 25 30 35 40

M2N2O1Q1K1, P1K2

alia

s p

erio

d (

day

s)

Satellite Repeat Period

• S1 and S2 aliased to zero frequency and hence contaminate mean circulation

• K1 and P1 aliased to annual and K2 to semiannual per iods

annual

semiannual

Internal tides from altimetry

Wavenumber spectrum100 km

Ray & Mitchum (1997)

Besides the intr insic science of internal tides, they introduce 1-5 cm/sec error in ocean current velocity at mesoscales.

Two key issues for OSTST to consider

• The choice of orbit: Although a sun-synchronous orbit has significant cost and technical benefits, the tidal aliasing problem will significantly reduce the value of the mission to oceanographic applications. Do we need any fur ther studies before putting this issue to bed? (to be discussed in the Tide Splinter )

• The wet tropospher ic correction in coastal oceans: As the inter ferometry technique is able to provide SSH meaurements next to the coast line, the land contamination of the microwave radiometer observations will limit the accuracy of wet-tropospher ic correction for high-resolution coastal applications.