14.03.2015 Views

open file - Viru Peipsi

open file - Viru Peipsi

open file - Viru Peipsi

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

Changes in Water<br />

Level and Storage in<br />

Lakes<br />

Water level Decrease the flooded<br />

areas surround of lakes<br />

during the higher water<br />

period<br />

Storage of lakes Increase of total and<br />

active storage of lakes<br />

during winter period<br />

Possible decrease the<br />

level in the end of<br />

summer under the<br />

optimal level<br />

Conclusions<br />

In general, all climate change scenarios for Estonia forecast mild winters, a<br />

decrease in snow cover and an increase in the duration of dry periods in mid–<br />

summer. The predicted global warming will cause more changes in the water<br />

balance elements in the cold period than in the warm season. Modelled<br />

annual runoff and its seasonal variability in study area are not very sensitive<br />

to climate change. The main results of the study are following:<br />

• Periodical fluctuations of water level and river runoff. Long time<br />

series of annual precipitation has a significant periodicity of 25–35<br />

years in Estonia during more than a century. It causes long-term<br />

fluctuations in hydrological regime and alternation of wet and dry<br />

periods also in the future.<br />

• Increase in annual runoff. Due to the climate change, annual runoff<br />

will increase by 20–40 % in the average, for the year 2100, but<br />

modelled river runoff show a great spatial variation.<br />

• Significant increase in winter runoff. During mild winters, duration of<br />

snow and ice cover should decrease, winter weather should be<br />

changed more unstable, freezing and melting periods should<br />

alternate.<br />

• Decrease of spring runoff maximum and its shift earlier. Mild winters<br />

cause faster melting of snow and earlier beginning of spring<br />

hydrological season. Frequent melting periods in winter prevent big<br />

accumulation of snow. The mean maximum runoff should move<br />

from April to March.<br />

• Increase of river runoff in autumn. This is directly caused by<br />

significant increase of autumn precipitation predicted by both of the<br />

GCMs. In East-Estonia autumn maximum runoff would not exceed<br />

maximum runoff in spring.<br />

• Lengthening of the period of minimum runoff in summer. Due to<br />

faster melting of snow, decreasing and moving earlier of runoff<br />

maximum in spring, dry period should begin earlier. Minimum runoff<br />

period when rivers receive the majority of water from groundwater,

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!