Abstract
Conventional ocean-viewing radar altimeters (RA) have inherent limitations that become especially apparent when considering applications in the coastal environment. This chapter looks at three new technologies, two of which are to be on forthcoming missions: the delay-Doppler (or SAR mode) altimeter, to be embarked on CryoSat-2 and Sentinel-3, and Alti-Ka, on India’s SARAL mission (previously Oceansat-3). These instruments are nadir-viewing, each featuring a smaller footprint, improved tracking, and finer measurement precision. Wide swath techniques also are reviewed, represented by KaRIn. That concept offers altimetric coverage over an area that extends nominally 80 km to both sides of its nadir track. Relative to coastal applications, all three approaches have their respective advantages and limitations, highlighted in the discussion.
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Notes
- 1.
See Chapter by Benveniste, this volume.
- 2.
See Chapter by Dufau et al., this volume.
- 3.
See Chapter by Ray et al., this volume.
- 4.
See Chapter by Benveniste, this volume.
- 5.
By international spectral allocation agreements, this bandwidth is the largest available for space-based earth observation at Ka-band.
- 6.
If Eq. 20.3 is recast in terms of temporal range resolution τ, the resulting expression is equivalent to the classic form, except for Walsh’s Earth curvature term 1/a (Eq. 20.2). Walsh introduced that factor to scale spacecraft velocity V into the surface footprint velocity, which was not a correct rendition of the underlying physics.
- 7.
From this point of view, the PRF upper bound may be seen as the obverse of the Nyquist sampling criterion, which states that to assure pulse-to-pulse correlation the sampling rate must be larger than the bandwidth of the (complex) spectrum being sampled.
- 8.
- 9.
See Chapter by Gommenginger et al., this volume.
- 10.
Abbreviations
- CTE:
-
Coefficient of Thermal Expansion
- DDA:
-
Delay-Doppler Altimeter
- DEM:
-
Digital Elevation Model
- DORIS:
-
Doppler Orbitography and Radiopositioning Integrated by Satellite
- EM:
-
ElectroMagnetic
- FFT:
-
Fast Fourier Transform
- GAMBLE:
-
Global Altimeter Measurements By Leading Europeans
- JPL:
-
Jet Propulsion Laboratory
- KaRIN:
-
Ka-band Radar INterferometer
- KaSOARI:
-
Ka-band Swath Ocean Altimetry with Radar Interferometry
- POD:
-
Precision Orbit Determination
- PRF:
-
Pulse-Repetition Frequency
- RA:
-
Conventional non-coherent Radar Altimeter
- RAR:
-
Real Aperture Radar
- SAR:
-
Synthetic Aperture Radar
- SARAL:
-
Satellite with ARgos and ALtika
- SIRAL-2:
-
SAR/Interferometric Radar ALtimeter
- SRTM:
-
Shuttle Radar Topography Mission
- SRAL:
-
SAR Radar ALtimeter
- SSH:
-
Sea Surface Height
- SWH:
-
Significant Wave Height
- SWOT:
-
Surface Water and Ocean Topography
- WITTEX:
-
Water Inclination Topography and Technology EXperiment
- WS:
-
Wind Speed
- WSOA:
-
Wide Swath Ocean Altimeter
- WVR:
-
Water-Vapor Radiometer
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Raney, R.K., Phalippou, L. (2011). The Future of Coastal Altimetry. In: Vignudelli, S., Kostianoy, A., Cipollini, P., Benveniste, J. (eds) Coastal Altimetry. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-12796-0_20
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