FN Archimer Export Format PT J TI GNSS-R nonlocal sea state dependencies: Model and empirical verification BT AF CHEN-ZHANG, David D. RUF, Christopher S. ARDHUIN, Fabrice PARK, Jeonghwan AS 1:1;2:2;3:3;4:4; FF 1:;2:;3:;4:; C1 Univ Michigan, Dept Elect & Comp Engn, Ann Arbor, MI 48109 USA. Univ Michigan, Climate & Space Dept, Ann Arbor, MI 48109 USA. Univ Brest, IFREMER, Lab Ocean Phys & Satellite Oceanog, CNRS,IRD, Plouzane, France. Ohio State Univ, Electrosci Lab, Columbus, OH 43212 USA. C2 UNIV MICHIGAN, USA UNIV MICHIGAN, USA CNRS, FRANCE UNIV OHIO STATE, USA UM LOPS IF 2.939 TC 14 UR https://archimer.ifremer.fr/doc/00358/46909/46809.pdf LA English DT Article DE ;waves;wind;remote sensing AB Global Navigation Satellite System Reflectometry (GNSS-R) is an active, bistatic remote sensing technique operating at L-band frequencies. GNSS-R signals scattered from a rough ocean surface are known to interact with longer surface waves than traditional scatterometery and altimetry signals. A revised forward model for GNSS-R measurements is presented which assumes an ocean surface wave spectrum that is forced by other sources than just the local near-surface winds. The model is motivated by recent spaceborne GNSS-R observations that indicate a strong scattering dependence on significant wave height, even after controlling for local wind speed. This behavior is not well represented by the most commonly used GNSS-R scattering model, which features a one-to-one relationship between wind speed and the mean-square-slope of the ocean surface. The revised forward model incorporates a third generation wave model that is skillful at representing long waves, an anchored spectral tail model, and a GNSS-R electromagnetic scattering model. In comparisons with the spaceborne measurements, the new model is much better able to reproduce the empirical behavior. PY 2016 PD NOV SO Journal Of Geophysical Research-oceans SN 2169-9275 PU Amer Geophysical Union VL 121 IS 11 UT 000392841000024 BP 8379 EP 8394 DI 10.1002/2016JC012308 ID 46909 ER EF