Zobrazeno 1 - 10
of 30
pro vyhledávání: '"Dennis Booge"'
Autor:
Birgit Quack, Dennis Booge, Helmke Hepach, Elliot Atlas, Josefine Karnatz, Alexandra Rosa, Claudio Cardoso, Stephen Ball, Philippe Potin, Rüdiger Röttgers
Short-lived bromo-, chloro- and iodocarbons from marine and anthropogenic sources contribute to the atmospheric halogen budgets and to ozone depletion in the troposphere and stratosphere. Their spatial variations are poorly known, given the sparse ob
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aa506f74520dc67767df3987736edc69
https://doi.org/10.5194/egusphere-egu23-6381
https://doi.org/10.5194/egusphere-egu23-6381
Carbon disulfide (CS2) is one of the most important precursors for atmospheric carbonyl sulphide (OCS), a climate relevant trace gas that can serve as a proxy to quantify terrestrial gross primary production. Currently, limited understanding of the p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4e1ec2a57b9f4cf062ea1e3af7b900b7
https://doi.org/10.5194/egusphere-egu23-9269
https://doi.org/10.5194/egusphere-egu23-9269
Bromoform (CHBr3) is one of the most important precursors of atmospheric reactive bromine with an atmospheric lifetime of ~20 days. Natural production, being the main source of oceanic CHBr3, is high at the coasts and in open ocean upwelling regions
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::499f83c802a74ca0673ab8e1560ecd01
https://doi.org/10.5194/egusphere-egu23-12225
https://doi.org/10.5194/egusphere-egu23-12225
Climate-relevant trace gas air–sea exchange exerts an important control on air quality and climate, especially in remote regions of the planet such as the Southern Ocean. It is clear that polar regions exhibit seasonal trends in productivity and bi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d663b4c1cb2bc46b834699974e505c6e
https://doi.org/10.5194/bg-2022-106
https://doi.org/10.5194/bg-2022-106
Methane (CH4) is a climate-relevant atmospheric trace gas which is emitted to the atmosphere from coastal areas such as the Baltic Sea. The oceanic CH4 emission estimates are still associated with a high degree of uncertainty partly because the tempo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::20a567ed97d210f42cb4b72653604388
https://bg.copernicus.org/articles/19/4993/2022/
https://bg.copernicus.org/articles/19/4993/2022/
Methane (CH4) is a climate-relevant atmospheric trace gas which is emitted to the atmosphere from coastal areas such as the Baltic Sea. The oceanic CH4 emission estimates are still associated with a high degree of uncertainty partly because the tempo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::197824531c9c3ba3b9753c05a9325e0b
https://doi.org/10.5194/egusphere-2022-325
https://doi.org/10.5194/egusphere-2022-325
Autor:
Christa A. Marandino, Xiaobin Xu, Elliot Atlas, Sinikka T. Lennartz, Huixiang Xie, Heinz Bingemer, Rafel Simó, Kazushi Aranami, Meinrat O. Andreae, Pau Cortes, Birgit Quack, Andrew Marriner, Cliff S. Law, Stefanie Kremser, Gregory A. Cutter, G Uher, Max Berkelhammer, Dennis Booge, Marc von Hobe
Publikováno v:
Earth System Science Data. 12:591-609
Carbonyl sulfide (OCS) and carbon disulfide (CS2) are volatile sulfur gases that are naturally formed in seawater and exchanged with the atmosphere. OCS is the most abundant sulfur gas in the atmosphere, and CS2 is its most important precursor. They
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1c44fb20d8d9910ece3dd49614136e56
https://doi.org/10.5194/essd-12-591-2020
https://doi.org/10.5194/essd-12-591-2020
Autor:
Christa A. Marandino, Hermann W. Bange, Astrid Bracher, Cathleen Schlundt, Yanan Zhao, Jonathan Williams, Dennis Booge, Elliot Atlas
Publikováno v:
Biogeosciences, Vol 19, Pp 701-714 (2022)
Biogeosciences
Biogeosciences
Our understanding of the biogeochemical cycling of the climate-relevant trace gas dimethyl sulfide (DMS) in the Peruvian upwelling system is still limited. Here we present oceanic and atmospheric DMS measurements which were made during two shipborne
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1c4eee72707d55395a27844c589aaf68
https://bg.copernicus.org/articles/19/701/2022/bg-19-701-2022.html
https://bg.copernicus.org/articles/19/701/2022/bg-19-701-2022.html
Autor:
Miming Zhang, Dennis Booge, Jinpei Yan, Suqing Xu, Chen Liang, Yanfang Wu, Bo Yang, Jianjun Wang, Jun Zhao, Dong Li, Jianming Pan, Keyhong Park
Highlights: • Ultrahigh seawater DMS levels (>40 nM) were detected near the Antarctic Peninsula. • Ultrahigh DMS was only found in waters of algal bloom and abundant microzooplankton. • Grazing of abundant microzooplankton possibly cause the ul
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e7c409bd8c6a4256d6be73b435ab7b73
https://doi.org/10.1016/j.pocean.2022.102744
https://doi.org/10.1016/j.pocean.2022.102744