Large discharges from ships in the Black Sea studied by synthetic aperture radar with the support of automated identification systems

2014 ◽  
Vol 35 (14) ◽  
pp. 5513-5526 ◽  
Author(s):  
A. Yu. Ivanov ◽  
A.A. Kucheiko
2011 ◽  
Vol 139 (12) ◽  
pp. 3992-4000 ◽  
Author(s):  
Werner Alpers ◽  
Andrei Yu. Ivanov ◽  
Knut-Frode Dagestad

Abstract Foehn wind blowing through the Kolkhida (Kolkheti) Lowland in the southwestern Caucasus (western Georgia) was observed on an Envisat synthetic aperture radar (SAR) image as it encountered an atmospheric cyclonic eddy over the Black Sea on 13 September 2010. This SAR image reveals unprecedented finescale features of the near-surface wind fields that cannot be resolved by other sensors. It shows, among others, the deflection of the foehn wind by the atmospheric eddy. Quantitative information on the near-surface wind field over the sea is extracted from the SAR image.


2009 ◽  
Vol 137 (3) ◽  
pp. 1150-1161 ◽  
Author(s):  
Werner Alpers ◽  
Andrei Ivanov ◽  
Jochen Horstmann

Abstract Bora events over the Adriatic Sea and Black Sea are investigated by using synthetic aperture radar (SAR) images acquired by the advanced SAR (ASAR) on board the European satellite Envisat. It is shown that the sea surface roughness patterns associated with bora events, which are captured by SAR, yield information on the finescale structure of the bora wind field that cannot be obtained by other spaceborne instruments. In particular, SAR is capable of resolving 1) bora-induced wind jets and wakes that are organized in bands normal to the coastline, 2) atmospheric gravity waves, and 3) boundaries between the bora wind fields and ambient wind fields. Quantitative information on the sea surface wind field is extracted from the Envisat ASAR images by inferring the wind direction from wind-induced streaks visible on SAR images and by using the C-band wind scatterometer model CMOD_IFR2 to convert normalized cross sections into wind speeds. It is argued that spaceborne SAR images acquired over the east coasts of the Adriatic Sea and the Black Sea are ideal means to validate and improve mesoscale atmospheric models simulating bora events.


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