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locations of meteorological stations used in this study. The shaded background represents terrain height and sea depth in kilometers according to the scale on the right side. The "Bojana" mark shows position of the point where Bojana river enters the Adriatic Sea (this is also the border between Montenegro and Albania on the coast).}}{17}{figure.1}} \newlabel{terrain}{{1}{17}{The South Adriatic region with locations of meteorological stations used in this study. The shaded background represents terrain height and sea depth in kilometers according to the scale on the right side. The "Bojana" mark shows position of the point where Bojana river enters the Adriatic Sea (this is also the border between Montenegro and Albania on the coast)}{figure.1}{}} \HyPL@Entry{17<>} \@writefile{lof}{\contentsline {figure}{\numberline {2}{\ignorespaces Measured accumulated 24 hourly precipitation on rain guagues in southeastern Croatia (smaller sybols) and Montenegro (larger symbols) during November 2012. Precipitation shown for a certain day is measured at 6 UTC accumulated from the previous 24 hours. Only stations close to Adriatic are shown.}}{18}{figure.2}} \newlabel{raingauge}{{2}{18}{Measured accumulated 24 hourly precipitation on rain guagues in southeastern Croatia (smaller sybols) and Montenegro (larger symbols) during November 2012. Precipitation shown for a certain day is measured at 6 UTC accumulated from the previous 24 hours. Only stations close to Adriatic are shown}{figure.2}{}} \HyPL@Entry{18<>} \@writefile{lof}{\contentsline {figure}{\numberline {3}{\ignorespaces ERA Interim 850 hPa wind (colour of the vectors shows wind speed in m/s as on the colour bar below), geopotentiel (blue isolines) and temperature (red isolines) with measured aerosol optical thickness at 12 UTC 7 November 2010 from MODIS (circles) and OMI (squares), AOT is shown in colour according to the colour bar on the right.}}{19}{figure.3}} \newlabel{erai850}{{3}{19}{ERA Interim 850 hPa wind (colour of the vectors shows wind speed in m/s as on the colour bar below), geopotentiel (blue isolines) and temperature (red isolines) with measured aerosol optical thickness at 12 UTC 7 November 2010 from MODIS (circles) and OMI (squares), AOT is shown in colour according to the colour bar on the right}{figure.3}{}} \HyPL@Entry{19<>} \@writefile{lof}{\contentsline {figure}{\numberline {4}{\ignorespaces Measured accumulated 24 hourly precipitation on rain guagues in Croatia, Montenegro and Macedonia (circles), TRMM rainfall data (squares) and 8km ALADIN forecast data (shaded), the precipitation is accumulated for the period from 06 UTC on 8 until 06 UTC on 9 (top) and from 06 UTC on 9 until 06 UTC on 10 (bottom) November 2010. The correcponding rainguage data is shown in Fig~\ref {raingauge} as measured on 9 and 10 November 2010.}}{20}{figure.4}} \newlabel{rain1}{{4}{20}{Measured accumulated 24 hourly precipitation on rain guagues in Croatia, Montenegro and Macedonia (circles), TRMM rainfall data (squares) and 8km ALADIN forecast data (shaded), the precipitation is accumulated for the period from 06 UTC on 8 until 06 UTC on 9 (top) and from 06 UTC on 9 until 06 UTC on 10 (bottom) November 2010. The correcponding rainguage data is shown in Fig~\ref {raingauge} as measured on 9 and 10 November 2010}{figure.4}{}} \HyPL@Entry{20<>} \@writefile{lof}{\contentsline {figure}{\numberline {5}{\ignorespaces ERA Interim 10m wind (colour of the vectors shows wind speed in m/s as on the colour bar below), mean sea level pressure (blue) and cloudiness (shades of gray) for 12 UTC on 16 November 2010.}}{21}{figure.5}} \newlabel{eraiuvnp}{{5}{21}{ERA Interim 10m wind (colour of the vectors shows wind speed in m/s as on the colour bar below), mean sea level pressure (blue) and cloudiness (shades of gray) for 12 UTC on 16 November 2010}{figure.5}{}} \@writefile{lof}{\contentsline {figure}{\numberline {6}{\ignorespaces Measured wind speed (dark blue, scale on the left) and mean sea level pressure (red) reduced by 980 hPa (to fit the scale on the left) and wind direction (light blue in degrees from north clockwise, scale on the right) for November 2010 (Sv. Jure is marked as Biokovo in Fig~\ref {terrain}).}}{21}{figure.6}} \newlabel{wind}{{6}{21}{Measured wind speed (dark blue, scale on the left) and mean sea level pressure (red) reduced by 980 hPa (to fit the scale on the left) and wind direction (light blue in degrees from north clockwise, scale on the right) for November 2010 (Sv. Jure is marked as Biokovo in Fig~\ref {terrain})}{figure.6}{}} \HyPL@Entry{21<>} \@writefile{lof}{\contentsline {figure}{\numberline {7}{\ignorespaces Forecast 10m wind in 8km (top) and 2km (bottom) resolution and measured wind speed and direction (arrows) from MetOp ASCAT data (above the sea surface), SYNOP and automatic stations for 12 UTC on 16 (left) and 12 UTC on 17 (right) November 2010. Colour of the vectors shows wind speed in m/s as on the colour bars. Model data are shown as thin vectors on a denser grid in the background, measured wind is shown as thicker vectors on the location of measurement. }}{22}{figure.7}} \newlabel{wind16}{{7}{22}{Forecast 10m wind in 8km (top) and 2km (bottom) resolution and measured wind speed and direction (arrows) from MetOp ASCAT data (above the sea surface), SYNOP and automatic stations for 12 UTC on 16 (left) and 12 UTC on 17 (right) November 2010. Colour of the vectors shows wind speed in m/s as on the colour bars. Model data are shown as thin vectors on a denser grid in the background, measured wind is shown as thicker vectors on the location of measurement}{figure.7}{}} \HyPL@Entry{22<>} \@writefile{lof}{\contentsline {figure}{\numberline {8}{\ignorespaces Measured water levels of rivers in Montenegro and Skadar lake in October and November 2010 and climatological river run-off of Albanian rivers (embeded figure). Moraca and Crnojevica rivers are tributaries to the Skadar lake, Bojana river takes the outflow from the Skadar lake and flows into the Adriatic sea at the position marked as Bojana in Fig~\ref {terrain}.}}{23}{figure.8}} \newlabel{rivers}{{8}{23}{Measured water levels of rivers in Montenegro and Skadar lake in October and November 2010 and climatological river run-off of Albanian rivers (embeded figure). Moraca and Crnojevica rivers are tributaries to the Skadar lake, Bojana river takes the outflow from the Skadar lake and flows into the Adriatic sea at the position marked as Bojana in Fig~\ref {terrain}}{figure.8}{}} \HyPL@Entry{23<>} \@writefile{lof}{\contentsline {figure}{\numberline {9}{\ignorespaces Surface currents (vectors) and sea surface temperature (shaded background) from ROMS for 00 UTC on 11 (a), 15 (b) and 19 (c) November 2010.}}{24}{figure.9}} \newlabel{roms}{{9}{24}{Surface currents (vectors) and sea surface temperature (shaded background) from ROMS for 00 UTC on 11 (a), 15 (b) and 19 (c) November 2010}{figure.9}{}} \HyPL@Entry{24<>} \@writefile{lof}{\contentsline {figure}{\numberline {10}{\ignorespaces Trajectories of drifters released at 12 UTC 19 (a) and 12 UTC 26 October (b), 00 (c) and 12 (d) UTC 8, 00 (e) and 12 (f) UTC 9, 00 (g) and 12 (h) UTC 10 and 00 UTC 11 (i) November 2010. Trajectories initiated off different parts of a rectangle in southeast Adriatic are plotted in different colours.}}{25}{figure.10}} \newlabel{trajs}{{10}{25}{Trajectories of drifters released at 12 UTC 19 (a) and 12 UTC 26 October (b), 00 (c) and 12 (d) UTC 8, 00 (e) and 12 (f) UTC 9, 00 (g) and 12 (h) UTC 10 and 00 UTC 11 (i) November 2010. Trajectories initiated off different parts of a rectangle in southeast Adriatic are plotted in different colours}{figure.10}{}} \newlabel{LastPage}{{}{25}{}{}{}}