Zobrazeno 1 - 10
of 13
pro vyhledávání: '"T. W. Hilton"'
Autor:
M. E. Whelan, S. T. Lennartz, T. E. Gimeno, R. Wehr, G. Wohlfahrt, Y. Wang, L. M. J. Kooijmans, T. W. Hilton, S. Belviso, P. Peylin, R. Commane, W. Sun, H. Chen, L. Kuai, I. Mammarella, K. Maseyk, M. Berkelhammer, K.-F. Li, D. Yakir, A. Zumkehr, Y. Katayama, J. Ogée, F. M. Spielmann, F. Kitz, B. Rastogi, J. Kesselmeier, J. Marshall, K.-M. Erkkilä, L. Wingate, L. K. Meredith, W. He, R. Bunk, T. Launois, T. Vesala, J. A. Schmidt, C. G. Fichot, U. Seibt, S. Saleska, E. S. Saltzman, S. A. Montzka, J. A. Berry, J. E. Campbell
Publikováno v:
Biogeosciences, Vol 15, Pp 3625-3657 (2018)
For the past decade, observations of carbonyl sulfide (OCS or COS) have been investigated as a proxy for carbon uptake by plants. OCS is destroyed by enzymes that interact with CO2 during photosynthesis, namely carbonic anhydrase (CA) and RuBisCO,
Externí odkaz:
https://doaj.org/article/3abe44227def4ae2b6ef8bc9f3855fc8
Publikováno v:
Atmospheric Chemistry and Physics, Vol 16, Pp 3711-3726 (2016)
Carbonyl sulfide (COS) measurements are one of the emerging tools to better quantify gross primary production (GPP), the largest flux in the global carbon cycle. COS is a gas with a similar structure to CO2; COS uptake is thought to be a proxy for
Externí odkaz:
https://doaj.org/article/ac3eee80068a4a33b3524bed56d42793
Publikováno v:
Biogeosciences, Vol 11, Iss 2, Pp 217-235 (2014)
Global terrestrial atmosphere–ecosystem carbon dioxide fluxes are well constrained by the concentration and isotopic composition of atmospheric carbon dioxide. In contrast, considerable uncertainty persists surrounding regional contributions to
Externí odkaz:
https://doaj.org/article/3dd736aa47ea4f2cbfbb112d86018999
Publikováno v:
Biogeosciences, Vol 10, Iss 7, Pp 4607-4625 (2013)
We evaluate spatial structure in North American CO2 flux observations using a simple diagnostic land surface model. The vegetation photosynthesis respiration model (VPRM) calculates net ecosystem exchange (NEE) using locally observed temperature and
Externí odkaz:
https://doaj.org/article/967399f7ce2f4c61b7edf59c1abf2f89
Autor:
Laurel R. Fox, Barry Sinervo, Anthony R. Ambrose, Simone Des Roches, Helen Cooper, T. W. Hilton, Kevin C. Brown, Katharine L. Stuble
Publikováno v:
BioScience. 71:874-882
Field stations are platforms for documenting patterns and processes in ecosystems and are critical for understanding how anthropogenic climate change reshapes nature. Although networks of field stations have been used to identify patterns at continen
Autor:
Yuting Wang, Mary E. Whelan, T. W. Hilton, Nicholas C. Parazoo, Leander D. L. Anderegg, John Worden, Christian Frankenberg, Le Kuai, Roisin Commane, J. Elliott Campbell, Y. P. Shiga, Grayson Badgley
Where does the carbon released by burning fossil fuels go? Currently, ocean and land systems remove about half of the CO2 emitted by human activities; the remainder stays in the atmosphere. These removal processes are sensitive to feedbacks in the en
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::55398baad4314d8a230a9e4cc6ac1cfd
https://authors.library.caltech.edu/105714/
https://authors.library.caltech.edu/105714/
Publikováno v:
Biogeosciences. 11:217-235
Global terrestrial atmosphere–ecosystem carbon dioxide fluxes are well constrained by the concentration and isotopic composition of atmospheric carbon dioxide. In contrast, considerable uncertainty persists surrounding regional contributions to the
Publikováno v:
Biogeosciences. 10:4607-4625
We evaluate spatial structure in North American CO2 flux observations using a simple diagnostic land surface model. The vegetation photosynthesis respiration model (VPRM) calculates net ecosystem exchange (NEE) using locally observed temperature and
Carbonyl sulfide (COS) measurements are one of the emerging tools to better quantify gross primary production (GPP), the largest flux in the global carbon cycle. COS is a gas with a similar structure to CO2; COS uptake is thought to be a proxy for GP
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c8acae3acf870f1bb5b39fa91c7fbe57
https://doi.org/10.5194/acpd-15-21095-2015
https://doi.org/10.5194/acpd-15-21095-2015
Global terrestrial atmosphere-ecosystem carbon dioxide fluxes are well-constrained by the concentration and isotopic composition of atmospheric carbon dioxide. In contrast, considerable uncertainty persists surrounding regional contributions to the n
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::78e6ede85a983078f83826ab21a97c39
https://doi.org/10.5194/bgd-10-13753-2013
https://doi.org/10.5194/bgd-10-13753-2013