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Identifying the Origin of Anomalous High Tropospheric Ozone in the Ozonesonde Data at Uccle by Comparison with Nearby De Bilt
The ozonesonde stations at Uccle (Belgium) and De Bilt (Netherlands), separated by only 175 km, o...
R van Malderen, H de Backer, A Delcloo, M Allaart | Journal: Atmosphere-Ocean | Volume: 0 | Year: 2014 | First page: 1 | Last page: 15 | doi: 10.1080/07055900.2014.886552
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Attribution of typhoon-induced torrential precipitation in Central Vietnam, October 2020
In October 2020, Central Vietnam was struck by heavy rain resulting from a sequence of 5 tropical...
Luu LN, Scussolini P, Kew S, Philip S, Hariadi MH, Vautard R, Van Mai K, Van Vu T, Truong KB, Otto F, van der Schrier G., van Aalst, M. K. amd van Oldenborgh, G. J. | Journal: Climatic Change | Volume: 169 | Year: 2021 | First page: 1 | Last page: 21 | doi: https://doi.org/10.1007/s10584-021-03261-3
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Pathways and pitfalls in extreme event attribution
The last few years have seen an explosion of interest in extreme event attribution, the science o...
GJ van Oldenborgh, K van der Wiel, S Kew, S Philip, F Otto, R Vautard, A King, F Lott, J Arrighi, R Singh, M van Aalst | Journal: Climatic Change | Volume: 166 | Year: 2021 | First page: 13 | doi: 10.1007/s10584-021-03071-7
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Impact of climate model resolution on soil moisture projections in central-western Europe
Global climate models project widespread decreases in soil moisture over large parts of Europe. T...
EC van der Linden, RJ Haarsma, G van der Schrier | Journal: Hydrology and Earth System Sciences | Volume: 23 | Year: 2019 | First page: 191 | Last page: 206 | doi: 10.5194/hess-23-191-2019
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Insight into the May 2015 summit inflation event at Kīlauea Volcano, Hawai‘i
We use ground and space geodetic data to study surface deformation at Kīlauea Volcano from Januar...
Mark J.W.Bemelmans
Elske de Zeeuw - van Dalfsen
Michael P.Poland
Ingrid A.Johanson | Journal: Journal of Volcanology and Geothermal Research | Volume: 415 | Year: 2021 | First page: 107250 | doi: 10.1016/j.jvolgeores.2021.107250
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