Ледоход на всех пересекаемых водото

Ледоход на всех пересекаемых водотоках отсутствует и чаще лёд тает на месте.

Межень в течение лета, осени и зимы в среднем мало отличается по водности и

истощение грунтовой составляющей стока к концу осени - зимы пополняется поверхностной

составляющей от выпадения осадков холодного времени года. Вследствие этого уровни

и водность межени стабильны. Как правило, межень прерывается дождевыми паводками,

но в условиях зарегулированности бассейна значительные объёмы стока расходуются

на пополнения запруд и только дождевые паводки редкой повторяемости могут вызвать

подъёмы уровней воды и увеличение расходов воды до соразмерных с половодьем, но не

превышающими его.

Территория проектируемого объекта, за данными многолетних наблюдений, в

зону затопления от паводков, в том числе 1% обеспеченности, не попадала. /Донецкий

Региональный Центр Гидрометрологиии /.

Résultats (Anglais) 1:

Ice floes at all crossed streams and more ice melts in place.

Low during the summer, autumn and winter, on average, a little water and

the depletion of the soil component of the flow by the end of the autumn-winter is the superficial

part of the cold season precipitation. Consequently, the levels of

and water availability drought period, there are stable. As a rule, low flow is interrupted by rain floods,

but in conditions of considerable volumes of runoff basin regulation spent

to refill dams and flooding rain only a rare occurrence can cause

rises in water levels and water to increase commensurate with overflowing waters, but not

than his

. Territory of the project, the data of long-term observations, the

Flood inundation, including 1% security does not reach. /Donetsk Regional Centre Of Gidrometrologiii/

.

Résultats (Anglais) 2:

Ice drift on all watercourses crossed and there is no more ice melts in place. Mezhennaya during the summer, fall and winter average differs little water content and depletion of groundwater flow component to the end of autumn - winter replenished surface component of precipitation cold season. Consequently, the levels of conductivity and low water stable. As a rule, low water interrupted by rain floods, but in terms of regulated pool Photo significant amounts spent on recharge dams and only rare recurrence rain floods can cause rises in water levels and flow rates to increase commensurate with the flood, but not exceeding it. territory of the proposed facility, for these long-term observations in the flood zone flood, including 1% of security from falling. / Donetsk Regional Center Gidrometrologiii /.

Résultats (Anglais) 3:

Art print on canvas --- agniart.ru All crossed watercourses is missing and more ice melts on the spot. Lord salinification during summer, autumn and winter, on average there is little different in vorticity and

The depletion of groundwater flow to the end of autumn - winter is part of Lord surface from rainfall from cold time of the year. As a consequence, the levels and Lord водность межени are stable. As a general rule,ALOS salinification interrupted natural treasures, but in the Lord vagueness drainage basin significant amounts being spent on replenishment lord clearly visible and only rain floods rare recurrence pattern may cause

Climbing water levels and the increase in expenditure water up to commensurate with which usually smolder, but not exceeding his lord.lord Territory constructions object, with the multi-year monitoring data, the lord of the area flooding floods,Including 1% of minerals, does not come into contact. /Donetsk Regional Center lord Гидрометрологиии /.