Zobrazeno 1 - 10
of 89
pro vyhledávání: '"Manuela I Brunner"'
Autor:
Manuela I. Brunner, Eric Gilleland
Publikováno v:
Earth's Future, Vol 12, Iss 4, Pp n/a-n/a (2024)
Abstract Spatially compounding droughts and floods challenge water management and may become more severe in a warming climate. However, the influence of climate change on widespread hydrologic extremes remains largely unknown because they are neither
Externí odkaz:
https://doaj.org/article/621242eb578547c896e1e691a7253d41
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 6, Pp n/a-n/a (2024)
Abstract As droughts propagate both in time and space, their impacts increase because of changes in drought properties. Because temporal and spatial drought propagation are mostly studied separately, it is yet unknown how drought spatial extent and c
Externí odkaz:
https://doaj.org/article/4d1e0c893df54a4f82c6d5cd8aa449ea
Publikováno v:
Journal of Hydrology: Regional Studies, Vol 51, Iss , Pp 101608- (2024)
Study region: Apalachicola-Chattahoochee-Flint (ACF) Basin in the Southeast US Study focus: Operational rules of managed river systems are typically developed based on historical hydrology. This approach fails to consider alternative plausible hydrol
Externí odkaz:
https://doaj.org/article/1f65abba24524e4094f81ac758abbcbb
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 2, Pp n/a-n/a (2023)
Abstract Streamflow droughts are governed by different hydro‐meteorological processes, whose relative importance may change over time, with potential impacts on drought severity. Here, we assess changes in the importance of different hydrological d
Externí odkaz:
https://doaj.org/article/37d6180646214c9cad642e98975fa0ac
Autor:
Manuela I. Brunner, Daniel L. Swain, Raul R. Wood, Florian Willkofer, James M. Done, Eric Gilleland, Ralf Ludwig
Publikováno v:
Communications Earth & Environment, Vol 2, Iss 1, Pp 1-11 (2021)
The response of flood risk in Bavaria, Germany to increases in rainfall extremes in a warming climate is modulated by land surface processes below a precipitation threshold, but not above, suggest ensemble simulations with a hydrological model.
Externí odkaz:
https://doaj.org/article/897681986ffb4beb81429b56194dfee3
Autor:
Manuela I Brunner, Kerstin Stahl
Publikováno v:
Environmental Research Letters, Vol 18, Iss 3, p 034011 (2023)
Recurrent hydrological droughts (streamflow deficits) are highly impactful and challenge water management. Regional studies have provided some evidence of drought-rich periods at specific time scales. However, it is yet unclear where and when drought
Externí odkaz:
https://doaj.org/article/3611ac4d016443468c20e77f0e053580
Autor:
Elke Kellner, Manuela I. Brunner
Publikováno v:
Earth's Future, Vol 9, Iss 1, Pp n/a-n/a (2021)
Abstract Mountains, said to be the world's water towers, are central for the provision of downstream water demands. This provision service is strongly challenged by climate change associated with changes in runoff amount and seasonality caused by the
Externí odkaz:
https://doaj.org/article/7b0fe2c34cc44502acdc340426dbbc1c
Autor:
Manuela I Brunner, Svenja Fischer
Publikováno v:
Environmental Research Letters, Vol 17, Iss 10, p 104038 (2022)
Widespread floods that affect several catchments are associated with large damages and costs. To improve flood protection, a better understanding of the driving processes of such events is needed. Here, we assess how spatial flood connectedness varie
Externí odkaz:
https://doaj.org/article/518bc8a172ef46c5ae3b07c351f45d04
Wildfires have reached an unprecedented scale in the Northern Hemisphere. The summers of 2021 and 2022 demonstrated the destructive power of wildfires especially in Northern America and Southern Europe. Global warming indicates that fire seasons will
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::edc0631faa6a9d980945f72f1ad755e9
https://nhess.copernicus.org/preprints/nhess-2023-51/
https://nhess.copernicus.org/preprints/nhess-2023-51/
Streamflow elasticity is a simple approximation of how responsive a river is to precipitation. It is represented as a ratio of the expected percentage change in streamflow for a 1 % change in precipitation. Typically estimated for the annual median s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6d833e4f285fb3864a341e44811886d6
https://hess.copernicus.org/preprints/hess-2022-407/
https://hess.copernicus.org/preprints/hess-2022-407/