LEADER 03828nam 22009733a 450 001 9910367750503321 005 20250203235430.0 010 $a9783039217472 010 $a303921747X 024 8 $a10.3390/books978-3-03921-747-2 035 $a(CKB)4100000010106212 035 $a(oapen)https://directory.doabooks.org/handle/20.500.12854/59051 035 $a(ScCtBLL)8c3cc8bc-124a-4761-b60d-51170c625eab 035 $a(OCoLC)1163812725 035 $a(EXLCZ)994100000010106212 100 $a20250203i20192019 uu 101 0 $aeng 135 $aurmn|---annan 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 00$aSea Surface Roughness Observed by High Resolution Radar$fSusanne Lehner, Xiaofeng Li, Atsushi Fujimura, Alex Soloviev 210 1$aBasel, Switzerland :$cMDPI,$d2019. 215 $a1 electronic resource (202 p.) 311 08$a9783039217465 311 08$a3039217461 330 $aChanges in sea surface roughness are usually associated with a change in the sea surface wind field. This interaction has been exploited to measure sea surface wind speed by scatterometry. A number of features on the sea surface associated with changes in roughness can be observed by synthetic aperture radar (SAR) because of the change in Bragg backscatter of the radar signal by damping of the resonant ocean capillary waves. With various radar frequencies, resolutions, and modes of polarization, sea surface features have been analyzed in numerous campaigns, bringing various datasets together, thus allowing for new insights into small-scale processes at a larger areal coverage. This Special Issue aims at investigating sea surface features detected by high spatial resolution radar systems, such as SAR. 610 $adispersion curve filtering 610 $aSynthetic Aperture Radar 610 $aRADARSAT Constellation Mission (RCM) 610 $amarine X-band radar 610 $acompact polarization (CP) 610 $across-polarization 610 $aproper orthogonal decomposition 610 $arain 610 $aright circular horizontal polarization model 610 $asupport vector machines 610 $aSentinel-1 610 $awind speed 610 $awave height 610 $ahurricane 610 $aocean surface waves 610 $aSMAP 610 $aCopernicus 610 $asynthetic aperture radar 610 $aco-polarized phase difference 610 $asynthetic aperture radar (SAR) 610 $aoceans 610 $afetch- and duration-limited wave growth relationships 610 $aWake detection 610 $aair-sea interaction 610 $aphase-resolved wave fields 610 $awind 610 $aSAR 610 $aCoVe-Pol and CoHo-Pol models 610 $aBaltic Sea 610 $awind retrieval 610 $aocean surface wind speed retrieval 610 $aCMEMS 610 $adetectability model 610 $aright circular vertical polarization model 610 $ahurricane internal dynamical process 610 $aocean winds 610 $apolarimetry 610 $asea surface roughness 610 $aeyewall replacement cycles 610 $aGF-3 610 $adual-polarization 610 $aquad-polarized SAR 610 $atyphoon/hurricane-generated wind waves 610 $acoast and ocean observation 610 $aradar 610 $ageophysical model function (GMF) 610 $aDoppler radar 700 $aLehner$b Susanne$01786459 702 $aLi$b Xiaofeng 702 $aFujimura$b Atsushi 702 $aSoloviev$b Alex 801 0$bScCtBLL 801 1$bScCtBLL 906 $aBOOK 912 $a9910367750503321 996 $aSea Surface Roughness Observed by High Resolution Radar$94318146 997 $aUNINA