2 Assessment of Water Resources in Poland
29
0
500
1000
1500
2000
2500
3000
3500
4000
XI
XII
I
II
III
IV
V
VI
VII VIII IX
X
m 3. s -1
SQ
WQ
NQ
Fig. 2.8 Maximum (WQ), average (SQ), and minimum (NQ) monthly Vistula flows (in m 3. s −1 ) at
Tczew, 1951–2015 (own study based on the data from [2])
0
200
400
600
800
1000
1200
1400
1600
XI XII
I
II
III
IV
V
VI VII VIII IX
X
m 3. s -1
SQ
WQ
NQ
Fig. 2.9 Maximum (WQ), average (SQ) and minimal (NQ) monthly Oder flows (in m 3. s −1 ) at
Gozdowice, 1951–2015 (own study based on the data from [2])
Kundzewicz [41] believes that compared to other countries around the world, Poland
is not particularly vulnerable to global warming, but the problem of floods (mainly
pluvial) and droughts may increase.
Recent research indicates that extreme weather conditions should be expected.
Comparative analysis of colder years (1961–1990) and warmer years (1991–2015)
29
0
500
1000
1500
2000
2500
3000
3500
4000
XI
XII
I
II
III
IV
V
VI
VII VIII IX
X
m 3. s -1
SQ
WQ
NQ
Fig. 2.8 Maximum (WQ), average (SQ), and minimum (NQ) monthly Vistula flows (in m 3. s −1 ) at
Tczew, 1951–2015 (own study based on the data from [2])
0
200
400
600
800
1000
1200
1400
1600
XI XII
I
II
III
IV
V
VI VII VIII IX
X
m 3. s -1
SQ
WQ
NQ
Fig. 2.9 Maximum (WQ), average (SQ) and minimal (NQ) monthly Oder flows (in m 3. s −1 ) at
Gozdowice, 1951–2015 (own study based on the data from [2])
Kundzewicz [41] believes that compared to other countries around the world, Poland
is not particularly vulnerable to global warming, but the problem of floods (mainly
pluvial) and droughts may increase.
Recent research indicates that extreme weather conditions should be expected.
Comparative analysis of colder years (1961–1990) and warmer years (1991–2015)
