Climate Change Induced Seasonal Amplification of the Indian Ocean CO2 Sink
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
Ground-based and helicopter-borne geophysical characterization of an alpine rock glacier
openaire +2 more sources
Spatially refined satellite gravimetry captures human signatures in global terrestrial water storage trends. [PDF]
O'Neill MM, Rodell M, Loomis BD.
europepmc +1 more source
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
Joint inversion of transient electromagnetic and radiomagnetotelluric data for enhanced subsurface characterization. [PDF]
Ibraheem IM +4 more
europepmc +1 more source
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]
Isaya D +5 more
europepmc +1 more source
Nonlinear Release of Subinertial Diurnal Internal Tides Forms Spiral Internal Solitary Waves
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
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
Younger Dryas drought and IPO climate modulation during the Antarctic Cold Reversal in New Zealand. [PDF]
Ohneiser C +4 more
europepmc +1 more source

