Results 211 to 220 of about 66,486 (308)

Simulated Changes and Future Analogy Extent of Ocean Heat Content During the Mid‐Pliocene Warm Period

open access: yesGeophysical Research Letters, Volume 53, Issue 3, 16 February 2026.
Abstract In the present day, global oceans have absorbed most of the excess anthropogenic heat, abating surface temperature warming. The Mid‐Pliocene Warm Period (MPWP; ∼ ${\sim} $3.2 million years ago) offers an opportunity to understand how globally warmer climates store oceanic heat.
Harry J. Grosvenor   +3 more
wiley   +1 more source

Salt‐Freshwater Mixing and Submarine Groundwater Discharge in Sloping Unconfined Tidal Aquifers

open access: yesGeophysical Research Letters, Volume 53, Issue 3, 16 February 2026.
Abstract Previous studies have revealed the groundwater flow and salt transport in unconfined coastal aquifers in response to numerous factors. However, previous studies assumed a flat aquifer base, and it is unclear how a sloping aquifer base would affect the subsurface flow and salinity distributions.
Chengji Shen   +5 more
wiley   +1 more source

Local Land‐Atmosphere Interactions Precondition Moist and Dry Heatwaves Under Large‐Scale Subsidence Over the Indo‐Gangetic Plains

open access: yesGeophysical Research Letters, Volume 53, Issue 3, 16 February 2026.
Abstract Increase in pre‐monsoon heatwaves over the Indo‐Gangetic Plains (IGP) of India threatens life and ecosystems. We investigate the sufficiency of large‐scale anticyclones in forming moist and dry heatwaves by analysing local land‐atmospheric conditions prior to 10 heatwaves in IGP.
Manali Saha   +2 more
wiley   +1 more source

Evaluation of the CO2 sequestration potential of afforestation projects and secondary forests in two different climate zones of South America [PDF]

open access: yes, 2002
Benìtez-Ponce, P.C.   +7 more
core   +1 more source

More Rapid Reduction of Spring Snow Cover on the Western Tibetan Plateau by Emergent Constraint

open access: yesGeophysical Research Letters, Volume 53, Issue 3, 16 February 2026.
Abstract Snow cover is a critical component of climate, hydrological, and ecological systems, particularly in high‐altitude and high‐latitude regions. Global warming has driven substantial snow cover retreat, yet projections from climate models vary widely, hindering reliable climate change adaptation and policy planning.
Jianyu Wang   +10 more
wiley   +1 more source

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