Catchment-scale dissolved carbon concentrations and export estimates across six subarctic streams in northern Sweden

被引:54
作者
Giesler, R. [1 ]
Lyon, S. W. [2 ,3 ]
Morth, C-M. [4 ]
Karlsson, J. [1 ]
Karlsson, E. M. [5 ]
Jantze, E. J. [2 ,3 ]
Destouni, G. [2 ,3 ]
Humborg, C. [6 ]
机构
[1] Climate Impacts Res Ctr, Abisko, Sweden
[2] Bert Bolin Ctr Climate Res, Stockholm, Sweden
[3] Dept Phys Geog & Quaternary Geol, Stockholm, Sweden
[4] Dept Geol Sci, Stockholm, Sweden
[5] Purdue Univ, Sch Civil Engn, Ecol Sci & Engn Interdisciplinary Grad Program, W Lafayette, IN 47907 USA
[6] Dept Appl Environm Sci, Stockholm, Sweden
基金
瑞典研究理事会;
关键词
ORGANIC-CARBON; DIOXIDE SUPERSATURATION; BOREAL CATCHMENTS; RIVER DISCHARGE; CLIMATE-CHANGE; PERMAFROST; RELEASE; TUNDRA; LAKES; RESPIRATION;
D O I
10.5194/bg-11-525-2014
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Climatic change is currently enhancing permafrost thawing and the flow of water through the landscape in subarctic and arctic catchments, with major consequences for the carbon export to aquatic ecosystems. We studied stream water carbon export in several tundra-dominated catchments in northern Sweden. There were clear seasonal differences in both dissolved organic carbon (DOC) and dissolved inorganic carbon (DIC) concentrations. The highest DOC concentrations occurred during the spring freshet while the highest DIC concentrations were always observed during winter baseflow conditions for the six catchments considered in this study. Long-term trends for the period 1982 to 2010 for one of the streams showed that DIC concentrations has increased by 9% during the 28 yr of measurement while no clear trend was found for DOC. Similar increasing trends were also found for conductivity, Ca and Mg. When trends were discretized into individual months, we found a significant linear increase in DIC concentrations with time for September, November and December. In these subarctic catchments, the annual mass of C exported as DIC was in the same order of magnitude as DOC; the average proportion of DIC to the total dissolved C exported was 61% for the six streams. Furthermore, there was a direct relationship between total runoff and annual dissolved carbon fluxes for these six catchments. These relationships were more prevalent for annual DIC exports than annual DOC exports in this region. Our results also highlight that both DOC and DIC can be important in high-latitude ecosystems. This is particularly relevant in environments where thawing permafrost and changes to subsurface ice due to global warming can influence stream water fluxes of C. The large proportion of stream water DIC flux also has implications on regional C budgets and needs to be considered in order to understand climate-induced feedback mechanisms across the landscape.
引用
收藏
页码:525 / 537
页数:13
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