2004Tunnelling and Underground Space TechnologyRequires access

101. Water Balances of the Northern Catchments of Finland

Pertti Seuna, Jarmo Linjama

Open publisher page 0 citations

Abstract

This paper discusses the water balances of three basins in northern Finland, between latitudes 66 and 69°N. Drainage areas vary from 11.6 to 16.4 km2. The Vaha-Askanjoki basin is completely covered by forest, the Iittovuoma basin is practically treeless, and the Laanioja basin is covered by forest to a major extent. Otherwise, conditions are quite similar in all three basins. Discharges are measured continuously, precipitation on a daily basis, and snow water equivalent (SWE) once or twice a month. Data series are 25–45 years long. The average water balance components were P corrected = 640 mm, Q = 409 mm and ET = 231 mm. There was no trend in SWE in the north, but quite a strong decreasing trend in southern Finland (62°N). A slight increasing trend in the evapotranspiration of the two forested basins was seen. The estimation of true areal precipitation is the most critical parameter in water balance calculations.

About this research paper

What this paper is about

This paper discusses the water balances of three basins in northern Finland, between latitudes 66 and 69°N. Drainage areas vary from 11.6 to 16.4 km2. The Vaha-Askanjoki basin is completely covered by forest, the Iittovuoma basin is practically treeless, and the Laanioja basin is covered by forest to a major extent. Otherwise, conditions are quite similar in all three basins. Discharges are measured continuously, precipitation on a daily basis, and snow water equivalent (SWE) once or twice a month. Data series are 25–45 years long. The average water balance components were P corrected = 640 mm, Q = 409 mm and ET = 231 mm. There was no trend in SWE in the north, but quite a strong decreasing trend in southern Finland (62°N). A slight increasing trend in the evapotranspiration of the two forested basins was seen. The estimation of true areal precipitation is the most critical parameter in water balance calculations.

Why it matters

A significance statement is not available in the OpenAlex record.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

This paper discusses the water balances of three basins in northern Finland, between latitudes 66 and 69°N. Drainage areas vary from 11.6 to 16.4 km2. The Vaha-Askanjoki basin is completely covered by forest, the Iittovuoma basin is practically treeless, and the Laanioja basin is covered by forest to a major extent. Otherwise, conditions are quite similar in all three basins. Discharges are measured continuously, precipitation on a daily basis, and snow water equivalent (SWE) once or twice a month. Data series are 25–45 years long. The average water balance components were P corrected = 640 mm, Q = 409 mm and ET = 231 mm. There was no trend in SWE in the north, but quite a strong decreasing trend in southern Finland (62°N). A slight increasing trend in the evapotranspiration of the two forested basins was seen. The estimation of true areal precipitation is the most critical parameter in water balance calculations.

Key concepts: Evapotranspiration, Water balance, Structural basin, Precipitation, Hydrology (agriculture), Snow, Latitude, Drainage basin

Related papers

Back to paper searchBrowse research topicsOriginal source
101. Water Balances of the Northern Catchments of Finland — Research Paper | ScholarLens