ORIGINAL RESEARCH
A 3S-based Regional Terrestrial Carbon Cycle
Model in Luanhe Basin, China
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1
State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute
of Water Resources and Hydropower Research, No. 1 Fuxing Road, Haidian District, Beijing 100038,China
2
College of Environmental Science and Engineering, Donghua University, No. 2999 Renminbei Road,
Songjiang District, Shanghai 201620, China
3
School of Environment, Liaoning University, No. 66 Chongshan Middle Road, Huanggu District,
Shenyang 110036, China
4
College of Resource Environment and Tourism, Capital Normal University, No.105 West Third Ring Road North,
Haidian District, Beijing 100048 China
Submission date: 2023-01-09
Final revision date: 2023-04-18
Acceptance date: 2023-04-21
Online publication date: 2023-05-18
Publication date: 2023-07-21
Corresponding author
Fang Liu
China Institute of Water Resources and Hydropower Research, Room 948, Building 1, China Institute of Water Res, 10038, Beijing, China
Pol. J. Environ. Stud. 2023;32(4):3721-3737
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ABSTRACT
For a comprehensive response to climate change and low carbon development mode, the 3S-based
regional terrestrial carbon cycle model in Luanhe basin is constructed in accordance with componentbased
development strategy to identify carbon cycle evolution of terrestrial ecosystem under the
background of local changes, combining measured weather data, prototype observation data of soil
and plants as well as remote-sensing information in different spatial and temporal scales. The model
has the ability of describing canopy fluxes, net primary productivity, biomass allocation and turnover,
mortality, decomposition of soil organic matter and other dynamic processes. The carbon cycle evolution
in Luanhe Basin from 1995 to 2010 is simulated and analyzed. The results are shown as follows:
1) in the temporal scale, inter-annual change of leaf area index with a slight growth trend is larger
than that of net primary productivity (NPP), ground and underground biomass and soil carbon content;
2) There are obvious regional differences in spatial view, spatial distribution of results are consistent
with those of watershed plant and soil, displaying the characteristics that the above major variables
of mountainous regions in middle-upper reaches are greater than those of grassland meadows in the
upstream and plains in the downstream.