Extremely cold ocean temperatures in iron formation brine pools of snowball Earth. [PDF]
Lu K +4 more
europepmc +1 more source
Bridging Geomythology and Geospatial Analysis for Flood Risk Assessment in Tamil Nadu
ABSTRACT The need for more holistic and context‐aware approaches to flood‐risk assessment has become increasingly urgent with extreme climate change events faced globally. Modern models overlook the long‐term environmental knowledge incorporated in ancient literature, myths, and cultural memory as they rely primarily on hydrological and geospatial ...
Shrishti Kushwah +3 more
wiley +1 more source
The past, present, and future evolution of Aurora Subglacial Basin's subglacial drainage system. [PDF]
Hayden AM, Pelle T, Dow CF.
europepmc +1 more source
Glacier Mass Balance of Mullwitzkees, Hohe Tauern, Austria, from 2006/07-2010/11
The annual glacier mass balance of Mullwitzkees in Hohe Tauern is measured since 1.10.2006 with the direct glaciological method in the fixed date system (1.10. to 30. 09. of the following year).
Institute for Meteorology and Geophysics Innsbruck
core
Moment Tensor Inversion Reveals Diverse Mechanisms for Icequakes in Ross Ice Shelf Rift WR4
Abstract Prior studies have cataloged thousands of icequakes at Ross Ice Shelf (RIS) Western Rift 4 (WR4) and linked them to tidal cycles, thermal stress, and temperature fluctuations. Building on this foundation, we apply a full moment tensor inversion using Green's functions for a layered firn, ice, water and sediment model.
Farzaneh Aziz Zanjani +5 more
wiley +1 more source
Subaqueous evidence of the last glacial maximum and its termination in southern Patagonia. [PDF]
Fedotova A, Magnani MB.
europepmc +1 more source
Glacier Mass Balance of Mullwitzkees, Hohe Tauern, Austria, from 2006/07-2009/10
The annual glacier mass balance of Mullwitzkees in Hohe Tauern is measured since 1.10.2006 with the direct glaciological method in the fixed date system (1.10. to 30. 09. of the following year).
Institute for Meteorology and Geophysics Innsbruck
core
The U.S. Atlantic and Gulf Coastal Plain (CP) sediments are kilometers‐thick, low‐velocity deposits underlain by high‐velocity bedrock that create regional patterns of amplification and attenuation of ground motions. Capturing these effects is challenging because of the limited subsurface information available, particularly the shear wave velocity (VS)
Cassie Gann‐Phillips +5 more
wiley +1 more source
Westerly induced precipitation increase drives near-surface ground ice gain on the Tibetan Plateau despite warming. [PDF]
Zhao Y +10 more
europepmc +1 more source
Abstract Future global and regional mean sea level (MSL) changes have been widely quantified, yet projections of extreme sea level (ESL) remain limited, despite their substantial environmental and socioeconomic risks to densely populated coastal regions such as the marginal seas near China. Here, we use a high‐resolution (∼8 km) regional ocean model to
Yi Jin +3 more
wiley +1 more source

