Results 231 to 240 of about 131,619 (292)

Climate Change Induced Seasonal Amplification of the Indian Ocean CO2 Sink

open access: yesGeophysical Research Letters, Volume 53, Issue 19, 16 October 2026.
Abstract This study investigates changes in the mean and seasonal states of oceanic carbon uptake across the Indian Ocean (IO) using an improved, high‐resolution, observationally constrained long‐term (1980–2019) surface ocean pCO2 ${\text{pCO}}_{2}$ data product.
A. P. Joshi   +5 more
wiley   +1 more source

Different Orbital Controls on Detrital Magnetic Components in the Ninety‐East Ridge Since the Late Pleistocene

open access: yesGeophysical Research Letters, Volume 53, Issue 19, 16 October 2026.
Abstract Magnetic minerals preserved in marginal‐sea sediments can serve as distinct fingerprints for unraveling paleoenvironmental evolution. However, the forcing mechanisms that govern the transport and accumulation of individual magnetic minerals at orbital timescales remain poorly constrained.
Yulong Guan   +6 more
wiley   +1 more source

Water Storage Capacity Dynamics in Drained Boreal Peatlands: Responses to Rewetting and Climate Change

open access: yesGeophysical Research Letters, Volume 53, Issue 19, 16 October 2026.
Abstract Historical peatland drainage resulted in surface subsidence and reduced water storage capacity (WSC), a process that can be exacerbated by climate change. We assessed the effects of rewetting on WSC using mesocosm experiments in climate chambers, field measurements, and Interferometric Synthetic Aperture Radar (InSAR) analysis.
Shokoufeh Salimi   +2 more
wiley   +1 more source

Hydroseismograms at Gran Sasso aquifer, central Italy, for earthquake hydrology studies. [PDF]

open access: yesSci Rep
Isaya D   +5 more
europepmc   +1 more source

Nonlinear Release of Subinertial Diurnal Internal Tides Forms Spiral Internal Solitary Waves

open access: yesGeophysical Research Letters, Volume 53, Issue 19, 16 October 2026.
Abstract Earth's rotation imposes a dynamical barrier on the free propagation of internal tides at high latitudes, raising questions about the fate of tidal energy poleward of the critical latitude. Satellite observations reveal spiral internal solitary waves (ISWs) along the continental slope of the South Orkney Plateau.
Zenghao Jiang   +5 more
wiley   +1 more source

High‐ and Low‐Latitude Insolation Forcing Drives the Half‐Precession Cycle in Winter Arctic Sea Ice

open access: yesGeophysical Research Letters, Volume 53, Issue 19, 16 October 2026.
Abstract The half‐precession cycle is a key climatic signal in global climate system, linking high‐ and low‐latitude climate variability and bridging orbital‐ and millennial‐scale climate changes. While it characterizes tropical insolation, its origin in high‐latitude climate records remains unclear. Based on a transient climate simulation spanning the
Zhipeng Wu   +6 more
wiley   +1 more source

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