Details
| Original language | English |
|---|---|
| Pages (from-to) | 404-412 |
| Number of pages | 9 |
| Journal | Russian meteorology and hydrology |
| Volume | 32 |
| Issue number | 6 |
| Publication status | Published - Jun 2007 |
| Externally published | Yes |
Abstract
With reference to 2001-2005, the fluxes of dissolved organic matter (DOM) are analyzed in a water stream of the northern taiga subzone of continuous permafrost. Dynamics of hydroclimatic parameters is shown during a frost-free period. It is found that, in spite of a potential decrease in the DOM concentrations with the increased thickness of a seasonally thawed layer, one observes their direct dependence on the precipitation amount and part that enters the water stream. Seasonal variations in the DOM qualitative composition are determined. The basic DOM part exported from the watershed is observed during the regimes of a maximum water content (spring flooding and floods).
ASJC Scopus subject areas
- Environmental Science(all)
- Water Science and Technology
- Chemical Engineering(all)
- Fluid Flow and Transfer Processes
- Earth and Planetary Sciences(all)
- Atmospheric Science
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In: Russian meteorology and hydrology, Vol. 32, No. 6, 06.2007, p. 404-412.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - Role of Climate in Removing Dissolved Organic Matter from Cryolithozone Watersheds in Central Siberia
AU - Prokushkin, A. S.
AU - Guggenberger, G.
N1 - Funding information: The work was supported by the Russian Foundation for Basic Research (projects 03-04-48037 and 05-05-64208) and the European Scientific Foundation (ESF Exchange Grant 667).
PY - 2007/6
Y1 - 2007/6
N2 - With reference to 2001-2005, the fluxes of dissolved organic matter (DOM) are analyzed in a water stream of the northern taiga subzone of continuous permafrost. Dynamics of hydroclimatic parameters is shown during a frost-free period. It is found that, in spite of a potential decrease in the DOM concentrations with the increased thickness of a seasonally thawed layer, one observes their direct dependence on the precipitation amount and part that enters the water stream. Seasonal variations in the DOM qualitative composition are determined. The basic DOM part exported from the watershed is observed during the regimes of a maximum water content (spring flooding and floods).
AB - With reference to 2001-2005, the fluxes of dissolved organic matter (DOM) are analyzed in a water stream of the northern taiga subzone of continuous permafrost. Dynamics of hydroclimatic parameters is shown during a frost-free period. It is found that, in spite of a potential decrease in the DOM concentrations with the increased thickness of a seasonally thawed layer, one observes their direct dependence on the precipitation amount and part that enters the water stream. Seasonal variations in the DOM qualitative composition are determined. The basic DOM part exported from the watershed is observed during the regimes of a maximum water content (spring flooding and floods).
UR - http://www.scopus.com/inward/record.url?scp=34548669149&partnerID=8YFLogxK
U2 - 10.3103/S1068373907060088
DO - 10.3103/S1068373907060088
M3 - Article
AN - SCOPUS:34548669149
VL - 32
SP - 404
EP - 412
JO - Russian meteorology and hydrology
JF - Russian meteorology and hydrology
SN - 1068-3739
IS - 6
ER -