Results 191 to 200 of about 184,697 (288)

Why forests can mitigate floods of all sizes: Evaluating the scientific basis for forest-based flood mitigation. [PDF]

Ambio
Kaluarachchi S, Alila Y.
europepmc   +1 more source

Plurality in transformative change: Three co‐created pathways toward nature‐positive Europe(s)

People and Nature, EarlyView.
Abstract The accelerating decline of biodiversity necessitates transformative change to protect nature and society, which requires innovative actions and governance strategies. This paper advances the conceptual understanding of transformative change by identifying patterns of change in three co‐created transformative pathways for a nature‐positive ...
Mara de Pater, Aniek Hebinck, Symke Nieboer, Anita Lazurko, Robbert Biesbroek, Laura Pereira, Elizabeth Díaz‐General, Aron Teunissen, Samia Baadj, Anna Chilton, Seweryn Krupnik, Richard Kock, Klemetti Näkkäläjärvi, W. Mathijs Rozemuller, Eirini Sakellari   +14 more
wiley   +1 more source

Towards more reliable interdisciplinary modelling of global human–environment dynamics driving biodiversity change

People and Nature, EarlyView.
Abstract Environmental problems are typically vast, urgent and complex. Confronted with such problems, we are often tempted to act fast by pulling together little bits and pieces from different fields and simply adding these to pre‐existing models and frameworks.
Carsten Meyer
wiley   +1 more source

Maximum water stress is decoupled from climate, traits, and growth in a xeric oak. [PDF]

New Phytol
Anderegg LDL, Skelton RP, Diaz J, Papper P, Lovegreen P, Trugman AT, Ackerly DD, Dawson TE.   +7 more
europepmc   +1 more source

Internal Permafrost Structure of Geomorphologically Distinct Palsas in Northern Sweden Revealed by Quasi‐3D ERT

Permafrost and Periglacial Processes, EarlyView.
ABSTRACT Permafrost in northern peatlands occurs within individual palsas or extensive peat plateaus and controls local carbon storage. These permafrost landforms are complex, and their internal structure remains poorly understood. We used quasi‐3D electrical resistivity tomography (ERT) measurements, supported by UAV‐LiDAR topography, frost probing ...
Cas Renette, Mirko Pavoni, Mauricio Fuentes, Erik Sturkell, Mats Olvmo, Heather Reese   +5 more
wiley   +1 more source

Effects of chemical and hydrological stress on the wing morphology of a damselfly. [PDF]

Environ Entomol
Mauser KM, Paudel S, Sigmund O, Entling MH, Ott J, Brühl CA.   +5 more
europepmc   +1 more source

Depositional and Hydrological Relationships Between Buried Dead Ice and the Active Layer in the McMurdo Dry Valleys, Antarctica: A Study of Sediment Geochemistry and Cation Concentrations

Permafrost and Periglacial Processes, EarlyView.
ABSTRACT The McMurdo Dry Valleys, the largest ice‐free region in Antarctica, are home to a cold‐desert hydrologic system of glaciers, snowbanks, streams, and lakes. Freshwater is also stored as dead glacial ice, which is poorly constrained in terms of ion concentrations and interactions with both in situ and overlying sediments.
Matthew C. Witscheber, Kate M. Swanger
wiley   +1 more source

New horizons in statistical downscaling and AI approaches for sustainable km-scale climate simulations. [PDF]

NPJ Clim Atmos Sci
Chun KP, Aragão L, Olmo ME, Nguyen VD, Risanto CB, Bettolli ML, Ezber Y, Toker E, Varotsos KV.   +8 more
europepmc   +1 more source

Quantifying the Surface Deformation of Pingos on the Alaskan North Slope Using Interferometric Synthetic Aperture Radar (InSAR)

Permafrost and Periglacial Processes, EarlyView.
ABSTRACT Pingos are large mounds with cores formed of intrusive ice that form in periglacial landscapes. These ice structures can form in regions of discontinuous permafrost, commonly as hydraulic or open‐system pingos, or in locations of continuous permafrost, commonly as hydrostatic or closed‐system pingos.
Venezia M. Follingstad, Roger J. Michaelides, Matthew R. Siegfried, Tyler M. Meng, John Bradford, Kynan H. G. Hughson, Alexia R. Kubas, Andrew Mullen, Enrica Quartini, Austin Routt, Hanna G. Sizemore, Andrei Swidinsky, Britney E. Schmidt   +12 more
wiley   +1 more source

Afforestation does not increase the temperature sensitivity of soil organic carbon decomposition in the water-level fluctuation zone. [PDF]

Front Plant Sci
Lei Y, Zhang W, Zhao J, Shuai H, Lou J, Fan X, Xu T, Dong H, Kumar A, Yu Z, Li H, Lin J.   +11 more
europepmc   +1 more source