LAKE 2.0: a model for temperature, methane, carbon dioxide and oxygen dynamics in lakes

A one-dimensional (1-D) model for an enclosed basin (lake) is presented, which reproduces temperature, horizontal velocities, oxygen, carbon dioxide and methane in the basin. All prognostic variables are treated in a unified manner via a generic 1-D transport equation for horizontally averaged prope...

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Bibliographic Details
Main Authors: V. Stepanenko, I. Mammarella, A. Ojala, H. Miettinen, V. Lykosov, T. Vesala
Format: Article
Language:English
Published: Copernicus Publications 2016-05-01
Series:Geoscientific Model Development
Online Access:http://www.geosci-model-dev.net/9/1977/2016/gmd-9-1977-2016.pdf
Description
Summary:A one-dimensional (1-D) model for an enclosed basin (lake) is presented, which reproduces temperature, horizontal velocities, oxygen, carbon dioxide and methane in the basin. All prognostic variables are treated in a unified manner via a generic 1-D transport equation for horizontally averaged property. A water body interacts with underlying sediments. These sediments are represented by a set of vertical columns with heat, moisture and CH<sub>4</sub> transport inside. The model is validated vs. a comprehensive observational data set gathered at Kuivajärvi Lake (southern Finland), demonstrating a fair agreement. The value of a key calibration constant, regulating the magnitude of methane production in sediments, corresponded well to that obtained from another two lakes. We demonstrated via surface seiche parameterization that the near-bottom turbulence induced by surface seiches is likely to significantly affect CH<sub>4</sub> accumulation there. Furthermore, our results suggest that a gas transfer through thermocline under intense internal seiche motions is a bottleneck in quantifying greenhouse gas dynamics in dimictic lakes, which calls for further research.
ISSN:1991-959X
1991-9603