Meteorological responses of carbon dioxide and methane fluxes in the terrestrial and aquatic ecosystems of a subarctic landscape

• Published in: Biogeosciences 2023-02, Vol.20 (3), p.545-572
• Main Authors: Heiskanen, Lauri, Tuovinen, Juha-Pekka, Vekuri, Henriikka, Räsänen, Aleksi, Virtanen, Tarmo, Juutinen, Sari, Lohila, Annalea, Mikola, Juha, Aurela, Mika
• Format: Article
• Language: English
• Subjects: Aquatic ecosystems; Atmosphere; Atmospheric carbon dioxide; Bogs; Carbon dioxide; Carbon dioxide flux; Climate change; Coniferous forests; Drought; Drought effects; Ecosystems; Ecotones; Eddy covariance; Emissions; Environmental aspects; Fens; Fluxes; Forest ecosystems; Forests; Groundwater table; Growing season; Heat waves; Ice; Lake sediments; Lakes; Landscape; Meteorological conditions; Methane; Microbalances; Moisture content; Moisture effects; Organic sediments; Peatlands; Permafrost; Plant stress; Precipitation; Primary production; Recovery time; Remote sensing; Respiration; Sediment; Soil moisture; Soil moisture content; Soil stresses; Summer; Terrestrial ecosystems; Uptake; Vapor pressure; Vapour pressure; Vegetation; Water content; Water table; Weather
• ISSN: 1726-4189; 1726-4170; 1726-4189
• DOI: 10.5194/bg-20-545-2023

The subarctic landscape consists of a mosaic of forest, peatland, and aquatic ecosystems and their ecotones. The carbon (C) exchange between ecosystems and the atmosphere through carbon dioxide (CO2) and methane (CH4) fluxes varies spatially and temporally among these ecosystems. Our study area in Kaamanen in northern Finland covered 7 km2 of boreal subarctic landscape with upland forest, open peatland, pine bogs, and lakes. We measured the CO2 and CH4 fluxes with eddy covariance and chambers between June 2017 and June 2019 and studied the C flux responses to varying meteorological conditions. The landscape area was an annual CO2 sink of −45 ± 22 and −33 ± 23 g C m−2 and a CH4 source of 3.0 ± 0.2 and 2.7 ± 0.2 g C m−2 during the first and second study years, respectively. The pine forest had the largest contribution to the landscape-level CO2 sink, −126 ± 21 and −101 ± 19 g C m−2, and the fen to the CH4 emissions, 7.8 ± 0.2 and 6.3 ± 0.3 g C m−2, during the first and second study years, respectively. The lakes within the area acted as CO2 and CH4 sources to the atmosphere throughout the measurement period, and a lake located downstream from the fen with organic sediment showed 4-fold fluxes compared to a mineral sediment lake. The annual C balances were affected most by the rainy peak growing season in 2017, the warm summer in 2018, and a heatwave and drought event in July 2018. The rainy period increased ecosystem respiration (ER) in the pine forest due to continuously high soil moisture content, and ER was on a level similar to the following, notably warmer, summer. A corresponding ER response to abundant precipitation was not observed for the fen ecosystem, which is adapted to high water table levels, and thus a higher ER sum was observed during the warm summer 2018. During the heatwave and drought period, similar responses were observed for all terrestrial ecosystems, with decreased gross primary productivity and net CO2 uptake, caused by the unfavourable growing conditions and plant stress due to the soil moisture and vapour pressure deficits. Additionally, the CH4 emissions from the fen decreased during and after the drought. However, the timing and duration of drought effects varied between the fen and forest ecosystems, as C fluxes were affected sooner and had a shorter post-drought recovery time in the fen than forest. The differing CO2 flux response to weather variations showed that terrestrial ecosystems can have a contrasting impact on the land