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Ocean wave spectra in tropical cyclones with the Earth Explorer 10 candidate Harmony Marcel Kleinherenbrink, Paco Lopez-Dekker, Bertrand Chapron, Alexis Mouche

Ocean wave spectra in tropical cyclones with the Earth

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Page 1: Ocean wave spectra in tropical cyclones with the Earth

Ocean wave spectra in tropical cyclones with the Earth Explorer 10 candidate Harmony

Marcel Kleinherenbrink, Paco Lopez-Dekker, Bertrand Chapron, Alexis Mouche

Page 2: Ocean wave spectra in tropical cyclones with the Earth

Harmony observation concept: Stereo phase

→ 3D surface deformation (dInSAR).

→ Ocean surface motion (Doppler).

→ Surface winds (scatterometry).

→ Improved surface wave spectra (NRCS modulation).

→ Sea surface temperature (TIR).

→ Cloud-top motion and height (TIR time-lapse/parallax).

Page 3: Ocean wave spectra in tropical cyclones with the Earth

Harmony observation concept: XTI phase

→ 3D surface deformation.

→ Surface elevation time-series:- Glaciers- Permafrost- Icebergs- Volcanoes

→ Ocean topography.

Page 4: Ocean wave spectra in tropical cyclones with the Earth

4

Mission Timeline

Y1 Y2 Y3 Y4 Y5

Ice Volume change Ice Volume change

Glacier dynamics Glacier dynamics

3-D Ice surface motion

Air-sea interactions

Exp. Ocean topography Atmosphere-ocean-extemes (Tropical Cyclones, Polar lows, etc) Exp. Ocean topography

Upper ocean dynamics

Tectonic Strain

Vol. change (volcanoes) Vol. change (volcanoes)

Iceberg volume Sea-ice instantaneous motion/deformation Iceberg motion

Page 5: Ocean wave spectra in tropical cyclones with the Earth

Monostatic ‘equivalent’

300-400 kmS1 HH

~20º~20º

M.E. M.E. Top view

Three lines-of-sight

→ Polarimetric rotation.→ Bragg wave number change.→ Non-perp. Doppler/range.

→ Scatterometers: low-resolution.→ SAR: single line-of-sight.→ Planes: limited coverage.

300-400 km

Harmony: high-resolution three lines-of-sight Doppler and backscatter.

Page 6: Ocean wave spectra in tropical cyclones with the Earth

SAR distortions→ RAR modulation:

→ Surface tilt.→ Hydrodynamics.→ Range bunching.

→ SAR distortion:→ Velocity bunching.→ Azimuthal cut-off.

Gunson and Lehner, 2001

Page 7: Ocean wave spectra in tropical cyclones with the Earth

Tropical cyclone wave modeling

→ Kudryavtsev et al. (2021a/b).→ Numerically grow wave trains in a wind field.→ ‘Wave spectra’ estimated in the red box.

Page 8: Ocean wave spectra in tropical cyclones with the Earth

Tropical cyclone waves

→ Inflow angle: 20 deg → Inflow angle: 5 deg

Significant wave height [m]

Wave spectra contain information about the wind field.

Page 9: Ocean wave spectra in tropical cyclones with the Earth

Tropical cyclone wave modeling

Page 10: Ocean wave spectra in tropical cyclones with the Earth

SAR observations

TC Jose, courtesy of Huimin Li and Alexis Mouche

Page 11: Ocean wave spectra in tropical cyclones with the Earth

RAR wave spectraSwell Wind wavesSwell

Wind waves

Page 12: Ocean wave spectra in tropical cyclones with the Earth

SAR wave spectraSwell

Wind waves

Page 13: Ocean wave spectra in tropical cyclones with the Earth

SAR spectral coverage

Page 14: Ocean wave spectra in tropical cyclones with the Earth

Summary

→ Harmony’s multi-target mission:→ Ocean and air-sea interactions (currents, waves, wind, clouds).→ Cryosphere (sea ice, land ice, icebergs).→ Solid Earth (strain, volcanoes).

→ Tropical cyclones:→ Harmony has three lines-of-sight:

→ High-resolution Doppler.→ High-resolution backscatter.

→ Harmony’s SAR spectra:→ Improved spectral coverage.→ Improved contraints on wave spectra.