期刊
LIMNOLOGY AND OCEANOGRAPHY LETTERS
卷 3, 期 3, 页码 236-245出版社
WILEY
DOI: 10.1002/lol2.10070
关键词
-
资金
- US National Science Foundation [DEB-1440297, EAR-0725019, DEB-1517823]
- Direct For Biological Sciences
- Division Of Environmental Biology [1440297] Funding Source: National Science Foundation
- Direct For Computer & Info Scie & Enginr
- Div Of Information & Intelligent Systems [1344272] Funding Source: National Science Foundation
The rate at which water and carbon move through lake-catchments influences carbon metabolism, storage, and transport to down-stream ecosystems. This article focuses on conceptual-mathematical modeling of the age of water and carbon in lake-catchment systems, where age is defined as the time since the water parcel and environmental tracer entered the system. We test a framework for implementing models and data for the Lake Mendota lake-catchment system. We show that the lake-catchment system provides the basis for predicting time varying age of carbon along flow paths, and the residence times of dissolved organic carbon (DOC) leaving each compartment, which further helps to provide a deeper understanding of fundamental biogeochemical dynamic processes of carbon and water cycling within the lake-catchment system. Three scenarios illustrate how the age of DOC might evolve from climate or land cover change that alters the hydrologic water balance through increases or decreases in lake-catchment precipitation and evapotranspiration.
作者
我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。
推荐
暂无数据