Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Laura Thölix"'
Autor:
Laura Thölix, Leif Backman, Minttu Havu, Cécile de Munck, Valéry Masson, Leena Järvi, Olli Nevalainen, Esko Karvinen, Liisa Kulmala
Solutions to reduce carbon dioxide (CO2) emissions and to achieve carbon neutrality have become an important subject. Thus, there is a growing interest in accelerating also the carbon sinks of urban vegetation and finding the best practices for desig
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b6bf3a687796e0af1bfd02a0d71d2822
https://doi.org/10.5194/egusphere-egu22-4805
https://doi.org/10.5194/egusphere-egu22-4805
The climate in the Boreal area is warming at a pace that is exceeding the global average. Both temperature and precipitation is projected to increase due to climate change. The gross primary production in the forested area is also projected to increa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::00d2d88b0ccdd1290c5a44e451221652
https://doi.org/10.5194/egusphere-egu21-16030
https://doi.org/10.5194/egusphere-egu21-16030
Publikováno v:
Atmospheric Chemistry and Physics, Vol 18, Pp 15047-15067 (2018)
Stratospheric water vapour influences the chemical ozone loss in the polar stratosphere via control of the polar stratospheric cloud formation. The amount of water vapour entering the stratosphere through the tropical tropopause differs substantially
Autor:
David W. Tarasick, Quentin Errera, Laura Thölix, Samuel J. Oltmans, Shima Bahramvash Shams, Bryan J. Johnson, Von P. Walden, Irina Petropavlovskikh, Patrick Cullis, Rigel Kivi, Chance W. Sterling
Publikováno v:
Atmospheric Chemistry and Physics, Vol 19, Pp 9733-9751 (2019)
Understanding variations in atmospheric ozone in the Arctic is difficult because there are only a few long-term records of vertical ozone profiles in this region. We present 12 years of ozone profiles from February 2005 to February 2017 at four sites
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b007eac6ddc9ef3fff386fe12488cd9f
https://www.atmos-chem-phys.net/19/9733/2019/
https://www.atmos-chem-phys.net/19/9733/2019/
Radionuclides 137Cs and 90Sr and total beta activity were determined from air filters collected in Rovaniemi (Finnish Lapland) in1965–2011. Nuclear contamination sources present in the air filter samples as well as temporal changes in radionuclide
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4096c40cc41a10d91d8632b2a40339ab
http://hdl.handle.net/10138/304575
http://hdl.handle.net/10138/304575
Publikováno v:
Environmental Science and Pollution Research International
Radionuclides 137Cs and 90Sr and total beta activity were determined from air filters collected in Rovaniemi (Finnish Lapland) in 1965–2011. Nuclear contamination sources present in the air filter samples as well as temporal changes in radionuclide
Publikováno v:
Atmospheric Chemistry and Physics, Vol 16, Pp 4307-4321 (2016)
This study evaluates the stratospheric water vapour distribution and variability in the Arctic. A FinROSE chemistry climate model simulation covering years 1990–2013 is compared to observations (satellite and frostpoint hygrometer soundings) and th
Autor:
Rigel Kivi, Laura Thölix, Von P. Walden, Patrick Cullis, Bryan J. Johnson, Shima Bahramvash Shams, Quentin Errera, Samuel J. Oltmans, Irina Petropavlovskikh, Chance W. Sterling
Understanding the drivers of atmospheric ozone variations in the Arctic is difficult because there are few long-term records of vertical ozone profiles in this region. We present 12 years of ozone profiles over Summit Station, Greenland (72.6 N, 38.4
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bf2638fa80d87e6217cebfe2065e77ae
https://doi.org/10.5194/acp-2018-620
https://doi.org/10.5194/acp-2018-620
Stratospheric water vapor plays a key role in radiative and chemical processes, it e.g. influences the chemical ozone loss via controlling the polar stratospheric cloud formation in the polar stratosphere. The amount of water entering the stratospher
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ea848cccb96caeb12eb35f7a43486f82
https://doi.org/10.5194/acp-2018-310
https://doi.org/10.5194/acp-2018-310