Results 61 to 70 of about 953 (168)
Eun Jin Lee, Eunyup Lee, Miyoung Kim, Han-Sung Kim, Young Kyung Lee, and Hee Jung Kang Department of Laboratory Medicine, Hallym University Sacred Heart Hospital, Hallym University College of Medicine, Anyang, Korea Background: For convenience, multiple ...
Eun Jin Lee +5 more
semanticscholar +1 more source
Abstract The East Antarctic Ice Sheet (EAIS) formed circa 34 million years ago and now contains an ice volume equivalent to ∼52 m of global sea‐level rise. Although the EAIS is approximately in balance today, there is substantial uncertainty regarding the sensitivity of sectors underlain by low‐lying bed topography to future climate and ocean warming ...
Guy J. G. Paxman +5 more
wiley +1 more source
External Quality Assessment of Institutions and Instruments Using a Linear Mixed Model
Jinsook Lim, Sungho Won, Suyeon Park, Jimyung Kim, Sun Hoe Koo, and Gye Choel Kwon Department of Laboratory Medicine, Chungnam National University Hospital, Daejeon; Department of Public Health Science, Graduate School of Public Health, Seoul National ...
Jinsook Lim +5 more
semanticscholar +1 more source
Increased Glacier Melt Across Millennia to Hours Enhances Erosion and Sediment Export Processes
Abstract Glacial erosion and sediment evacuation are key in shaping polar and mountain landscapes and influencing downstream ecological and social systems. The glacier dynamics and hydrology responsible for these processes are closely linked to hydrological and climatic (hydro‐climatic) conditions.
Ian Delaney +11 more
wiley +1 more source
ABSTRACT Only one last interglacial relative sea‐level indicator point (SLIP) has been recognised for Fenland, eastern England, and the nearest penultimate interglacial SLIP is located on the north Norfolk coast. Such limited information restricts the regional input to, and hence the relevance of, global reconstructions of late Middle and Late ...
H. E. Langford +7 more
wiley +1 more source
Three Drivers of 21st‐Century Changes in Ocean Tides
Abstract Numerical model simulations are conducted to study the response of barotropic ocean tides to 21st‐century climate change, as manifested by sea level rise, increasing ocean stratification, and expanding Antarctic ice shelf cavities. Emphasis is placed on surface elevations, with projections of M2 ${\mathrm{M}}_{2}$, S2 ${\mathrm{S}}_{2}$, K1 ${\
Lana Opel +8 more
wiley +1 more source
Abstract Whillans Ice Plain (WIP), a region of West Antarctica flowing into the southern Ross Sea, lurches forward 0.2–0.6 m over 30–60 min once or twice per diurnal ocean tidal cycle. Combining 11 years (2008–2019) of 30 s or better resolution Global Navigation Satellite System (GNSS) data from past field campaigns is necessary to provide insight into
Z. S. Katz, M. R. Siegfried, L. Padman
wiley +1 more source
An integrated Structure-from-Motion and time-lapse technique for quantifying ice-margin dynamics
Fine resolution topographic data derived from methods such as Structure from Motion (SfM) and Multi-View Stereo (MVS) have the potential to provide detailed observations of geomorphological change, but have thus far been limited by the logistical ...
JOSEPH MALLALIEU +4 more
doaj +1 more source
Winter Baseflow Calibration's Critical Role in Hydrological Modeling for the Pamir Region
Abstract The Pamir Mountains, a critical water source for Central Asia, require accurate quantification of runoff components for water resource management under climate change. Uncertainties in precipitation data are known to greatly affect hydrological model accuracy, leading to the widespread use of multi‐data calibration methods to avoid internal ...
J. Huang +4 more
wiley +1 more source
Repeat laser scanning and change detection revealed that large but infrequent rockfall events dominated summer debris supply from subaerial rock slopes bordering Miage Glacier, Italy. Rockfall source locations reflect the legacy of recent deglaciation and possibly longer‐term glacial trimlines, highlighting climate‐driven controls on sediment fluxes in
Rebecca Stewart +4 more
wiley +1 more source

