Zobrazeno 1 - 10
of 177
pro vyhledávání: '"L, Klemedtsson"'
Autor:
J. Rinne, P. Łakomiec, P. Vestin, J. D. White, P. Weslien, J. Kelly, N. Kljun, L. Ström, L. Klemedtsson
Publikováno v:
Biogeosciences, Vol 19, Pp 4331-4349 (2022)
The reasons for spatial and temporal variation in methane emission from mire ecosystems are not fully understood. Stable isotope signatures of the emitted methane can offer clues to the causes of these variations. We measured the methane emission (FC
Externí odkaz:
https://doaj.org/article/17c160f291a14a21975d94b39a038ec4
Publikováno v:
Biogeosciences, Vol 19, Pp 3921-3934 (2022)
We measured CO2 and CH4 fluxes using chambers and eddy covariance (only CO2) from a moist moss tundra in Svalbard. The average net ecosystem exchange (NEE) during the summer (9 June–31 August) was negative (sink), with −0.139 ± 0.032 µmol m−2
Externí odkaz:
https://doaj.org/article/2817d9856a514d59ba0e7c9bcd60dc4a
Autor:
R. Poyatos, V. Granda, V. Flo, M. A. Adams, B. Adorján, D. Aguadé, M. P. M. Aidar, S. Allen, M. S. Alvarado-Barrientos, K. J. Anderson-Teixeira, L. M. Aparecido, M. A. Arain, I. Aranda, H. Asbjornsen, R. Baxter, E. Beamesderfer, Z. C. Berry, D. Berveiller, B. Blakely, J. Boggs, G. Bohrer, P. V. Bolstad, D. Bonal, R. Bracho, P. Brito, J. Brodeur, F. Casanoves, J. Chave, H. Chen, C. Cisneros, K. Clark, E. Cremonese, H. Dang, J. S. David, T. S. David, N. Delpierre, A. R. Desai, F. C. Do, M. Dohnal, J.-C. Domec, S. Dzikiti, C. Edgar, R. Eichstaedt, T. S. El-Madany, J. Elbers, C. B. Eller, E. S. Euskirchen, B. Ewers, P. Fonti, A. Forner, D. I. Forrester, H. C. Freitas, M. Galvagno, O. Garcia-Tejera, C. P. Ghimire, T. E. Gimeno, J. Grace, A. Granier, A. Griebel, Y. Guangyu, M. B. Gush, P. J. Hanson, N. J. Hasselquist, I. Heinrich, V. Hernandez-Santana, V. Herrmann, T. Hölttä, F. Holwerda, J. Irvine, S. Isarangkool Na Ayutthaya, P. G. Jarvis, H. Jochheim, C. A. Joly, J. Kaplick, H. S. Kim, L. Klemedtsson, H. Kropp, F. Lagergren, P. Lane, P. Lang, A. Lapenas, V. Lechuga, M. Lee, C. Leuschner, J.-M. Limousin, J. C. Linares, M.-L. Linderson, A. Lindroth, P. Llorens, Á. López-Bernal, M. M. Loranty, D. Lüttschwager, C. Macinnis-Ng, I. Maréchaux, T. A. Martin, A. Matheny, N. McDowell, S. McMahon, P. Meir, I. Mészáros, M. Migliavacca, P. Mitchell, M. Mölder, L. Montagnani, G. W. Moore, R. Nakada, F. Niu, R. H. Nolan, R. Norby, K. Novick, W. Oberhuber, N. Obojes, A. C. Oishi, R. S. Oliveira, R. Oren, J.-M. Ourcival, T. Paljakka, O. Perez-Priego, P. L. Peri, R. L. Peters, S. Pfautsch, W. T. Pockman, Y. Preisler, K. Rascher, G. Robinson, H. Rocha, A. Rocheteau, A. Röll, B. H. P. Rosado, L. Rowland, A. V. Rubtsov, S. Sabaté, Y. Salmon, R. L. Salomón, E. Sánchez-Costa, K. V. R. Schäfer, B. Schuldt, A. Shashkin, C. Stahl, M. Stojanović, J. C. Suárez, G. Sun, J. Szatniewska, F. Tatarinov, M. Tesař, F. M. Thomas, P. Tor-ngern, J. Urban, F. Valladares, C. van der Tol, I. van Meerveld, A. Varlagin, H. Voigt, J. Warren, C. Werner, W. Werner, G. Wieser, L. Wingate, S. Wullschleger, K. Yi, R. Zweifel, K. Steppe, M. Mencuccini, J. Martínez-Vilalta
Publikováno v:
Earth System Science Data, Vol 13, Pp 2607-2649 (2021)
Plant transpiration links physiological responses of vegetation to water supply and demand with hydrological, energy, and carbon budgets at the land–atmosphere interface. However, despite being the main land evaporative flux at the global scale, tr
Externí odkaz:
https://doaj.org/article/c24e67cafe694cb3a5179d458e868fd8
Autor:
J. Jauhiainen, J. Alm, B. Bjarnadottir, I. Callesen, J. R. Christiansen, N. Clarke, L. Dalsgaard, H. He, S. Jordan, V. Kazanavičiūtė, L. Klemedtsson, A. Lauren, A. Lazdins, A. Lehtonen, A. Lohila, A. Lupikis, Ü. Mander, K. Minkkinen, Å. Kasimir, M. Olsson, P. Ojanen, H. Óskarsson, B. D. Sigurdsson, G. Søgaard, K. Soosaar, L. Vesterdal, R. Laiho
Publikováno v:
Biogeosciences, Vol 16, Pp 4687-4703 (2019)
Drained organic forest soils in boreal and temperate climate zones are believed to be significant sources of the greenhouse gases (GHGs) carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O), but the annual fluxes are still highly uncertain. Dr
Externí odkaz:
https://doaj.org/article/01e3c6406035494b87850b98504f82f7
Publikováno v:
Frontiers in Earth Science, Vol 8 (2021)
Globally peatlands store 500 Gt carbon (C), with northern blanket bogs accumulating 23 g C m−2 y−1 due to cool wet conditions. As a sink of carbon dioxide (CO2) peat bogs slow anthropogenic climate change, but warming climate increases the likeli
Externí odkaz:
https://doaj.org/article/8de39ace886a41ce9ff19f08a395f332
Publikováno v:
Geoscientific Model Development, Vol 11, Pp 725-751 (2018)
The symbiosis between plants and Ectomycorrhizal fungi (ECM) is shown to considerably influence the carbon (C) and nitrogen (N) fluxes between the soil, rhizosphere, and plants in boreal forest ecosystems. However, ECM are either neglected or pres
Externí odkaz:
https://doaj.org/article/1d5c08a2a6ca489eba58f47b31451475
Publikováno v:
SOIL, Vol 2, Iss 3, Pp 433-442 (2016)
The depolymerization of soil organic matter, such as proteins and (oligo-)peptides, into monomers (e.g. amino acids) is currently considered to be the rate-limiting step for nitrogen (N) availability in terrestrial ecosystems. The mineralization of f
Externí odkaz:
https://doaj.org/article/b8a46f3266c6422a959e334360d81773
Publikováno v:
Biogeosciences, Vol 13, Iss 8, Pp 2305-2318 (2016)
The CoupModel was used to simulate a Norway spruce forest on fertile drained peat over 60 years, from planting in 1951 until 2011, describing abiotic, biotic and greenhouse gas (GHG) emissions (CO2 and N2O). By calibrating the model against tree ring
Externí odkaz:
https://doaj.org/article/188853a012de4ec0befd3898fabd64f7
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Autor:
A. Meyer, L. Tarvainen, A. Nousratpour, R. G. Björk, M. Ernfors, A. Grelle, Å Kasimir Klemedtsson, A. Lindroth, M. Räntfors, T. Rütting, G. Wallin, P. Weslien, L. Klemedtsson
Publikováno v:
Biogeosciences, Vol 10, Iss 11, Pp 7739-7758 (2013)
Afforestation has been proposed as a strategy to mitigate the often high greenhouse gas (GHG) emissions from agricultural soils with high organic matter content. However, the carbon dioxide (CO2) and nitrous oxide (N2O) fluxes after afforestation can
Externí odkaz:
https://doaj.org/article/932de25938a94d0caef2900e9a67ea42