Dranse (Haute-Savoie)


The Dranse is a French river in the department of Haute-Savoie, that empties into Lake Geneva between Thonon-les-Bains and Évian-les-Bains.
The name "Dranse" comes from the former Drantia, based on the hydronym dur-, dora and the suffix -antia.

Geography

The Dranse is formed from the combination of three mountainous rivers originating from the peaks of the upper Chablais Alps, which converge upstream from the delta:
The Dranse d'Abondance is considered the higher-ordered stream of the Dranse. The Dranse de Morzine is consequently considered its tributary, according to Sandre, the French National Service for Water Data and Common Repositories Management.
The Dranse empties into Lake Geneva and forms a delta, which is integrated into the Delta de la Dranse National Nature Reserve, situated to the east of the commune of Thonon-les-Bains, which although small at an area of, offers an incomparable botanic diversity.
The river is long.
Whitewater kayakers and commercial rafting companies frequently run this river.

Hydrology

The Dranse is a high-volume river, as are all the rivers which originate in the Alpine mountain ranges. Its discharge was observed for a period of 97 years in Reyvroz, a locality in the department of Haute-Savoie situated on the southern bank of Lake Geneva at the same elevation as its outlet. The drainage basin for the river is in its totality, which is not quite three times the surface area of the city of Paris.
The annual average discharge of the river at Reyvroz is per second.
The Dranse is a typical seasonal river regime, with depends slightly on a small rain component. It exhibits sharply delineated seasonal fluctuations in discharge, which is characteristic of Alpine waterbodies. High flows occur in the springtime and are attributed to snowmelt. These accompany average monthly discharges of around per second from April to June. At the end of June, discharge rates sharply drop while the volume moves downstream. From the end of July to the end of February discharge is continuous, fluctuating between per second, with a low of in August, and a small "peak" cut in November, linked to the autumnal rain. However, these fluctuations are much more pronounced over short periods and depend on the year.
During times of low water, the low water discharge can fall as low as per second, in the case of a dry period, and although low, it is considered normal in the regions of the Alps and Prealps.
In terms of floods which, although uncommon, can be very important, measures with certain "eau du midi". The maximum instantaneous discharge for a two-year and five-year flood events are respectively. The ten-year flood event is per second, the twenty-year flood event , and the fifty-year flood .
The highest instantaneous flow recorded by the Reyvroz station was per second on the, while the maximum daily value was per second on. For comparison, the June 1963 value is comparable to a flood event, and is thus considered not that exceptional.
The discharge volume of Dranse is augmented by the abundant precipitation in the northern Alps. The runoff curve number for its drainage basin is annually, which elevated, is three times greater than the average for all of France. The specific discharge of the river reaches per second and square kilometer of the basin.