Results 121 to 130 of about 9,237 (223)
Wind-triggered Antarctic sea-ice decline preconditioned by thinning Winter Water. [PDF]
Spira T +6 more
europepmc +2 more sources
Evolution of Air‐Sea Fluxes in Modeled Long‐Lived Mesoscale Eddies in the South Atlantic Ocean
Abstract Mesoscale eddies modify physical and biogeochemical properties, facilitating the exchange of heat and CO2 between the surface, mixed‐layer and ocean interior. Most state‐of‐the‐art Earth System Models fail to resolve mesoscale processes O $O$(10–100 km) due to computational constraints, thus contributing to uncertainties in current and future ...
T. G. Smith +3 more
wiley +1 more source
Sea-ice proxies in Antarctic ice cores [PDF]
Röthlisberger, R., Abram, N.J.
openaire +2 more sources
Imminent Emergence of Permanent Surface Marine Heatwave States Across Global Oceans
Abstract Marine heatwaves (MHWs) can devastate ocean ecosystems, yet the timing at which anthropogenic changes in MHW characteristics permanently emerge from natural variability at the global scale remains poorly quantified. Here, we present the first global time of emergence analysis of MHW characteristics of the ocean surface using simulations from ...
Najmus Sadat Khan +7 more
wiley +1 more source
A schematic showing the links of tree‐scale (root‐, stem‐, and leaf‐level) and ecosystem‐scale water relations during the CSAD at CH‐Lae. Summary The summer of 2022 was characterized by compound soil and atmospheric drought (CSAD; low soil water content, SWC, and high vapor pressure deficit, VPD) in Central Europe, threatening forest carbon ...
Ankit Shekhar +19 more
wiley +1 more source
Abstract Hydrothermal systems at ultraslow‐spreading ridges are poorly understood, especially where thick sediments overlay detachment faults. The International Ocean Discovery Program Expedition 403 obtained the longest sediment record in Atlantic‐Arctic ultraslow‐spreading systems, reaching ∼628 m below the seafloor.
Y. Sakai +19 more
wiley +1 more source
Abstract The Atlantic Multidecadal Variability (AMV) influences North Atlantic sea surface temperatures and regional climate phenomena such as European droughts and hurricane activity. Its mechanisms remain complex due to long timescales and ocean‐atmosphere interactions.
Joakim Kjellsson, Wonsun Park
wiley +1 more source
Abstract Predicting the response of Antarctic ice to climate change requires detailed knowledge of its shallow structure, but direct measurements are challenging. Traditional seismic surveys are logistically demanding, and surface remote sensing provides limited information about subsurface layers.
Yibo Wang +5 more
wiley +1 more source
Abstract The sequence of events in the global carbon cycle during deglaciations is not entirely understood. Here, we analyze mean ocean δ13 ${\delta }^{13}$C and δ18 ${\delta }^{18}$O in an updated compilation of foraminiferal stable isotope data comprising 902 time series from 381 sediment cores, with individual records covering intervals within the ...
Peter Köhler, Stefan Mulitza
wiley +1 more source
Ocean carbon sequestration during glacial climates due to combined Antarctic sea ice expansion and ocean circulation change. [PDF]
Grégorio S +3 more
europepmc +1 more source

