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Full text: Negative storm surges in the Elbe estuary - Large-ScaleMeteorological conditions and future climate change

Atmosphere 2022, 13, 1634 
18 of 21 
Appendix A 
HE 
x 
N 
0 
x 
n 
20 
„30 L 
„40 
Storm 
Storm at negative storm surge 
J/V 
U/V at negative storm surge ® 
_ 
30 —20 —10 0 
= 
3 
% 
T—— — 
10 20 
30 
an 
N} 
A 
ln 
40 
* 
Le 
I 
Figure A1. Distribution of the U and V components of the geostrophic wind from the LWT classifica- 
ion for daily means (black) and for the 24-h mean before an ELW (red). Marked also is whether a 
gale was present at that time (blue and yellow ‘x’, respectively). 
Melgotand 
MAMA 
3 - —— ohservation 
— simulation | 
=] , ' ' 
14.03.2013 15.03.2018 16.03.2018 17.03.2018 18.03.2018 19.03.2018 20.03.2018 
MEZ 
Cuxhaven 
JakeAlphs 
AN AAN V 
A - ——ohservation 
— simulation | 
A N ' ' 
14.03.2018 15.03.2018 16.03.2018 17.03.2018 18.03.2018 19.03.2018 20.03.2018 
MEZ 
Brunsbuctlel 
y;— 
1 A 
70 \ x A | 
A 
| 
j ü 
VA X 1 N 
Ü 
A. — observation V V N \ W | 
— simulation | 
M 2, ' . 1 
14.03.2018 15.03.2018 16.03.2018 17.03.2018 18.03.2018 19.03.2018 20.03.2088 
MEZ 
Cneckstadt 
VA 
A 
„A 
R 
f 
RP 
1 -—— ohservation 
— simulation 
a . ; ; \ l 
14.03.2018 15.03.2018 18.03.2018 17,03.2018 18.03.2018 19.03.2018 20.03.2018 
rer 
A 
AMMAN. 
3 - — ohservation 
— simnlation 
#) 0 * ' ' \ 
14.03.2013 15.03.2018 16.03.2018 17.03.2018 13.03.2015 19.03.2018 20.03.2018 
MEZ 
Str Pauli 
A 
+ 
1 
‚NM 
A 
A 
x 
P 
4 
R 
u — 0ohse. tion 
— simulation * | 
wi ' 4 w 1 
24.03.2018 15.03.2018 16.03.2018 17.03.2018 18.03.2018 19.03.2018 20.03.2018 
MEZ 
Figure A2. Cont.
	        
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