Results 101 to 110 of about 39,293 (281)
Abstract Antarctic ice shelves control the flow of ice into the ocean, affecting the rate of sea level rise. This flow is regulated by ice‐shelf thickness, which depends on tributary flux across the grounding line and the balance between surface accumulation and ocean‐induced melting.
Vjeran Višnjević+5 more
wiley +1 more source
River ice responses to a warming Arctic—recent evidence from Russian rivers [PDF]
This paper looks at the response of river ice to recent warming in the Arctic at six major downstream gauges on large Russian rivers flowing to the Arctic Ocean.
Lammers, Richard B.+1 more
core +2 more sources
Modeling Daily Ice Cover in Northern Hemisphere Lakes With a Long Short‐Term Memory Neural Network
Abstract Quantifying lake ice loss is crucial for understanding the impact of climate change on lake ecosystems. In this study, we trained a deep learning model (Long‐Short Term Memory with Landsat observations, 1984–2012) to simulate Northern Hemisphere lake ice changes at a fine spatial scale >0.1km2 $\left( > \mathrm{0.1}\mathrm{k}{\mathrm{m ...
Xinchen He+5 more
wiley +1 more source
Analysis of current and historical data demonstrates that the cryosphere component are very sensitive to the climate change thus proving its role as the climate indicator. In the process of this a pattern of the changes clearly reflect regional climate characteristics.
openaire +2 more sources
The First Firn Core From the Cordillera Darwin Icefield: Implications for Future Ice Core Research
Abstract The Southern Hemisphere westerly winds (SHWWs) (45–65°S) are important regulators of the Southern Hemisphere climate. The scarcity of observational records at the core of the wind belt hinders our understanding of the environmental impact and long‐term variability of the westerly winds.
Dieter R. Tetzner+13 more
wiley +1 more source
Accurate ground-based datasets are important for correct interpretation of remote sensing data. West-Siberian Arctic has been exposed to rapid land-cover and land-use changes during the last 50 years.
Olga Khitun+4 more
doaj
Climate Feedbacks Derived From Spatial Gradients in Recent Climatology
Abstract Climate feedbacks, including Planck, surface albedo, water vapor‐lapse rate (WVLR) and cloud feedbacks, determine how much surface temperatures will eventually warm to balance anthropogenic radiative forcing. Climate feedbacks remain difficult to constrain directly from temporal variation in observed surface warming and radiation budgets due ...
P. Goodwin+3 more
wiley +1 more source
Abstract Present‐day ice‐mass changes in Antarctica typically deform the solid Earth elastically, and this signal needs removing from Global Positioning System (GPS) observations of displacement before they can be used to constrain models of glacial isostatic adjustment.
Grace A. Nield+6 more
wiley +1 more source
European Temperature Extremes Under Different AMOC Scenarios in the Community Earth System Model
Abstract Recent simulations using the Community Earth System Model (CESM) indicate that a tipping event of the Atlantic Meridional Overturning Circulation (AMOC) would cause Europe to cool by several degrees. This AMOC tipping event was found under constant pre‐industrial greenhouse gas forcing, while global warming likely limits this AMOC‐induced ...
René M. van Westen+1 more
wiley +1 more source
A new regional climate model for POLAR-CORDEX : evaluation of a 30-year hindcast with COSMO-CLM2 over Antarctica [PDF]
Continent-wide climate information over the Antarctic Ice Sheet (AIS) is important to obtain accurate information of present climate and reduce uncertainties of the ice sheet mass balance response and resulting global sea level rise to future climate ...
Demuzere, Matthias+7 more
core +2 more sources