RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 18, ES5005, doi:10.2205/2018ES000638, 2018

Figure 4. PDFs for a) – normalized radar cross-section $\sigma_0$; b) – significant wave height $H_s$; c) – wave period $T_{G03}$ for the model G03; d) – wave period $T_{\rm B14}$ for the model B14; e) – wave steepness for the model G03; f) – wave steepness for the model B14; g) – dimensionless wave height $gH_s/U_{\rm alt}^2) $ vs wave age $gT_{\rm G03}/(2\pi U_{\rm alt})$ for the model G03; h) – dimensionless wave height $gH_s/U_{\rm alt}^2) $ vs wave age $gT_{\rm B14}/(2\pi U_{\rm alt})$ for the model B14.

 
Citation: Badulin S., V. Grigorieva, A. Gavrikov, V. Geogjaev, M. Krinitskiy, M. Markina (2018), Wave steepness from satellite altimetry for wave dynamics and climate studies, Russ. J. Earth Sci., 18, ES5005, doi:10.2205/2018ES000638.
 

Copyright 2018 by the Geophysical Center RAS.