Results 151 to 160 of about 15,912 (215)
Resilience‐as‐doing: A relational model for living practice
Abstract Dominant frameworks treat resilience as a capacity to withstand disturbance and recover, something systems, communities or individuals either have or lack. This paper proposes a different understanding, grounded in relational onto‐epistemology and first‐person, practice‐based, autoethnographic inquiry situated within a household garden.
Katie Moon
wiley +1 more source
GIS-AHP-based land suitability assessment for sustainable agricultural planning on Qeshm Island. [PDF]
Darvishi A +5 more
europepmc +1 more source
ABSTRACT Due to its subsurface nature, permafrost cannot be directly observed with the naked eye or optical remote sensing. Consequently, accurately describing its distribution and thermal state is challenging. This is especially true in vast, remote environments, where obtaining comprehensive field data is demanding or improbable.
Ria Nicholson +5 more
wiley +1 more source
The chromosomal-level genome assembly and annotation of Phyllospadix iwatensis (Surfgrass). [PDF]
Wang J, Wang D, Zhao K, Liu Z, Zhang Q.
europepmc +1 more source
Repeated Pleistocene Permafrost Episodes in the Western Pannonian Basin
ABSTRACT Concerning the study of past periglacial processes, the Pannonian Basin is a key area as it contains the southernmost frost polygons found in Central Europe. The presence or absence of permafrost is still, however, a matter of debate, and data on the timing of frost action are also scarce.
Krisztina Sebe +5 more
wiley +1 more source
Tracing Marine Algal and Terrestrial Plant Inputs During Cenozoic Marine Incursions in the Northern Central Myanmar Basin: A Biomarker Perspective. [PDF]
Zhou Z, Shi Y, Yan T, Wang X.
europepmc +1 more source
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
West Antarctic Ice Sheet advance since the early Pliocene. [PDF]
Zhang M +17 more
europepmc +1 more source
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 +12 more
wiley +1 more source
Insolation-forced oceanic changes triggered the Eurasian Ice Sheet collapse and the Last Termination. [PDF]
Wu D +8 more
europepmc +1 more source

