Controls on snowmelt water mean transit times in northern boreal catchments

被引:59
作者
Lyon, Steve W. [1 ]
Laudon, Hjalmar [2 ]
Seibert, Jan [1 ,3 ]
Morth, Magnus [4 ]
Tetzlaff, Doerthe [5 ]
Bishop, Kevin H. [6 ]
机构
[1] Stockholm Univ, Dept Phys Geog & Quaternary Geol, S-10691 Stockholm, Sweden
[2] SLU, Dept Forest Ecol & Management, Umea, Sweden
[3] Univ Zurich, Dept Geog, Zurich, Switzerland
[4] Stockholm Univ, Dept Geol & Geochem, S-10691 Stockholm, Sweden
[5] Univ Aberdeen, Sch Geosci, Aberdeen, Scotland
[6] SLU, Dept Aquat Sci & Assessment, Uppsala, Sweden
基金
瑞典研究理事会;
关键词
mean transit time; catchment similarity; boreal systems; climate change; wetlands; snowmelt; RESIDENCE TIME; LANDSCAPE CHARACTERISTICS; RUNOFF GENERATION; RIVER DISCHARGE; FLOW; HYDROLOGY; SCALE; MODELS; HILLSLOPES; STREAMFLOW;
D O I
10.1002/hyp.7577
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Catchment-scale transit times for water are increasingly being recognized as an important control on geochemical processes. In this study, snowmelt water mean transit times (MTTs) were estimated for the 15 Krycklan research catchments in northern boreal Sweden. The snowmelt water MTTs were assumed to be representative of the catchment-scale hydrologic response during the spring thaw period and, as such, may be considered to be a component of the catchment's overall MTT. These snowmelt water MTTs were empirically related to catchment characteristics and landscape structure represented by using different indices of soil cover, topography and catchment similarity. Mire wetlands were shown to be significantly correlated to snowmelt MTTs for the studied catchments. In these wetlands, shallow ice layers form that have been shown to serve as impervious boundaries to vertical infiltration during snowmelt periods and, thus, alter the flow pathways of water in the landscape. Using a simple thought experiment, we could estimate the potential effect of thawing of ice layers on snowmelt hydrologic response using the empirical relationship between landscape structure (represented using a catchment-scale Pe number) and hydrologic response. The result of this thought experiment was that there could be a potential increase of 20-45% in catchment snowmelt water MTTs for the Krycklan experimental catchments. It is therefore possible that climatic changes present competing influences on the hydrologic response of northern boreal catchments that need to be considered. For example, MTTs may tend to decrease during some times of the year due to an acceleration in the hydrologic cycle, while they tend to increase MTTs during other times of the year due to shifts in hydrologic flow pathways. The balance between the competing influences on a catchment's MTT has consequences on climatic feedbacks as it could influence hydrological and biogeochemical cycles at the catchment scale for northern latitude boreal catchments. Copyright (C) 2010 John Wiley & Sons, Ltd.
引用
收藏
页码:1672 / 1684
页数:13
相关论文
共 68 条
[1]   Importance of seasonality and small streams for the landscape regulation of dissolved organic carbon export [J].
Agren, A. ;
Buffam, I. ;
Jansson, M. ;
Laudon, H. .
JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES, 2007, 112 (G3)
[2]  
Barnes CJ, 1996, HYDROL PROCESS, V10, P793, DOI 10.1002/(SICI)1099-1085(199606)10:6<793::AID-HYP372>3.0.CO
[3]  
2-K
[4]   Similarity analysis of subsurface flow response of hillslopes with complex geometry [J].
Berne, A ;
Uijlenhoet, R ;
Troch, PA .
WATER RESOURCES RESEARCH, 2005, 41 (09) :1-10
[5]  
Beven K.J., 1979, Hydrological Sciences Bulletin, V24, P43, DOI DOI 10.1080/02626667909491834
[6]   Resolving the Double Paradox of rapidly mobilized old water with highly variable responses in runoff chemistry [J].
Bishop, K ;
Seibert, J ;
Köher, S ;
Laudon, H .
HYDROLOGICAL PROCESSES, 2004, 18 (01) :185-189
[7]   THE ORIGINS OF ACID RUNOFF IN A HILLSLOPE DURING STORM EVENTS [J].
BISHOP, KH ;
GRIP, H ;
ONEILL, A .
JOURNAL OF HYDROLOGY, 1990, 116 (1-4) :35-61
[8]   Curvature distribution within hillslopes and catchments and its effect on the hydrological response [J].
Bogaart, P. W. ;
Troch, P. A. .
HYDROLOGY AND EARTH SYSTEM SCIENCES, 2006, 10 (06) :925-936
[9]   On the role of aspect to quantify water transit times in small mountainous catchments [J].
Broxton, Patrick D. ;
Troch, Peter A. ;
Lyon, Steve W. .
WATER RESOURCES RESEARCH, 2009, 45
[10]   THE UNIT RESPONSE OF GROUNDWATER OUTFLOW FROM A HILLSLOPE [J].
BRUTSAERT, W .
WATER RESOURCES RESEARCH, 1994, 30 (10) :2759-2763