Multimodel simulation of vertical gas transfer in a temperate lake

被引:23
作者
Guseva, Sofya [1 ,11 ]
Bleninger, Tobias [2 ]
Joehnk, Klaus [3 ]
Polli, Bruna Arcie [2 ]
Tan, Zeli [4 ]
Thiery, Wim [5 ,6 ]
Zhuang, Qianlai [7 ]
Rusak, James Anthony [8 ]
Yao, Huaxia [8 ]
Lorke, Andreas [1 ]
Stepanenko, Victor [9 ,10 ]
机构
[1] Univ Koblenz Landau, Inst Environm Sci, Landau, Germany
[2] Univ Fed Parana, Grad Program Water Resources & Environm Engn, Curitiba, Parana, Brazil
[3] CSIRO Land & Water Black Mt, Canberra, ACT 2601, Australia
[4] Pacific Northwest Natl Lab, Richland, WA 99352 USA
[5] Swiss Fed Inst Technol, Inst Atmospher & Climate Sci, Zurich, Switzerland
[6] Vrije Univ Brussel, Dept Hydrol & Hydraul Engn, Brussels, Belgium
[7] Purdue Univ, Dept Earth Atmospher & Planetary Sci, W Lafayette, IN 47907 USA
[8] Ontario Minist Environm Conservat & Parks, Dorset Environm Sci Ctr, Dorset, ON P0A 1E0, Canada
[9] Lomonosov Moscow State Univ, Res Comp Ctr, Lab Supercomp Modeling Climate Syst Proc, Moscow, Russia
[10] Lomonosov Moscow State Univ, Fac Geog, Dept Meteorol & Climatol, Moscow, Russia
[11] Lomonosov Moscow State Univ, Dept Geog, Moscow, Russia
基金
俄罗斯科学基金会;
关键词
METHANE EMISSIONS; CARBON-DIOXIDE; WATER TEMPERATURE; GREAT-LAKES; ICE COVER; DEEP LAKE; MODEL; CLIMATE; PERFORMANCE; PREDICTION;
D O I
10.5194/hess-24-697-2020
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
In recent decades, several lake models of varying complexity have been developed and incorporated into numerical weather prediction systems and climate models. To foster enhanced forecasting ability and verification, improvement of these lake models remains essential. This especially applies to the limited simulation capabilities of biogeo-chemical processes in lakes and greenhouse gas exchanges with the atmosphere. Here we present multi-model simulations of physical variables and dissolved gas dynamics in a temperate lake (Harp Lake, Canada). The five models (ALBM, FLake, LAKE, LAKEoneD, MTCR-1) considered within this most recent round of the Lake Model Intercomparison Project (LakeMIP) all captured the seasonal temperature variability well. In contrast, none of the models is able to reproduce the exact dates of ice cover and ice off, leading to considerable errors in the simulation of eddy diffusivity around those dates. We then conducted an additional modeling experiment with a diffusing passive tracer to isolate the effect of the eddy diffusivity on gas concentration. Remarkably, sophisticated kappa - epsilon models do not demonstrate a significant difference in the vertical diffusion of a passive tracer compared to models with much simpler turbulence closures. All the models simulate less intensive spring overturn compared to autumn. Reduced mixing in the models consequently leads to the accumulation of the passive tracer distribution in the water column. The lake models with a comprehensive biogeochemical module, such as the ALBM and LAKE, predict dissolved oxygen dynamics adequate to the observed data. However, for the surface carbon dioxide concentration the correlation between modeled (ALBM, LAKE) and observed data is weak (similar to 0.3). Overall our results indicate the need to improve the representation of physical and biogeochemical processes in lake models, thereby contributing to enhanced weather prediction and climate projection capabilities.
引用
收藏
页码:697 / 715
页数:19
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