Results 121 to 130 of about 3,056 (199)
Neogene Stable Carbon Isotopic Evolution of the Atmosphere and Low‐Latitude Surface Ocean
Abstract We reconstruct the stable carbon isotopic composition of Neogene surface ocean dissolved inorganic carbon (δ13CDIC) and atmospheric CO2 (δ13CATM) to serve as input for carbon cycle modeling and proxy‐related studies. The largely observation‐based δ13CDIC reconstructions are inferred from Neogene planktic foraminifer carbonate δ13C records with
J. A. van Dam +2 more
wiley +1 more source
Antarctic Sea‐Ice Loss Enhances East Asian Summer Precipitation Through Tropical Ocean Warming
Abstract Antarctic sea ice projected to have large reduction associated with increasing greenhouse gases, with potential impacts extending beyond the Southern Hemisphere. However, its influence on East Asian climate is not fully understood. Using Earth system model experiments and multi‐model simulations, we show that Antarctic sea‐ice loss by the end ...
Zhu Zhu +3 more
wiley +1 more source
Long range transport of South and East Asian anthropogenic aerosols counteracting Arctic warming
The large-scale convection during the Asian summer monsoon plays an important role in the rapid transport of boundary layer aerosols into the Asian summer monsoon anticyclone. Here, using the state-of-the-art ECHAM6–HAMMOZ aerosol-chemistry-climate model,
Suvarna Fadnavis +7 more
doaj +1 more source
This study examines the inter-annual variation of the difference in summer precipitation over the east and west side of the Ailao Mountain, as well as its relationship between the East Asia summer monsoon and the South Asia summer monsoon based on in ...
Yu LIAN, Yanyan XU, Huahong LI, Lei CAI
doaj +1 more source
Abstract Tropospheric ozone influences Earth's radiative energy budget and has increased in recent decades. With initial‐condition ensembles from a single chemistry‐climate model, we show that global surface anthropogenic NOx emissions explain about 90% of the simulated 1995–2014 tropospheric ozone increase (1.8 DU) and that this increase exceeds those
Xinyuan Yu +6 more
wiley +1 more source
Modeling a strong East Asian summer monsoon in a globally cool Earth, the MIS-13 case
International audienceDeep-sea and ice-core records show a significant reduced amplitude of the ice volume, temperature and greenhouse gases variations before Marine Isotope Stage (MIS) 11, about 400 000 years ago, with less warm (more glaciated ...
Goosse, H. +5 more
core
Abstract Mesoscale convective systems (MCSs) are known to induce heavy rainfall and pose significant weather hazards in tropical and mid‐latitude regions. Understanding the environmental conditions of MCSs is essential for improving model simulations and operational precipitation forecasts.
Shiwei Yu +5 more
wiley +1 more source
The Eurasian ice sheet reinforces the East Asian summer monsoon during the interglacial 500 000 years ago [PDF]
Deep-sea and ice-core records show that interglacial periods were overall less "warm" before about 420 000 years ago than after, with relatively higher ice volume and lower greenhouse gases concentration.
Qiuzhen Yin +5 more
doaj
Abstract Overshooting convection significantly impacts the composition of the upper troposphere and lower stratosphere (UTLS), yet its linkage to Atmospheric Rivers (ARs) remains poorly understood. This study investigates how ARs modulate environmental conditions and moisture distribution associated with overshooting convection in the central and ...
Ju‐Mee Ryoo +7 more
wiley +1 more source
. The acidity of precipitation has been observed at stations of the Acid Rain Monitoring Network run by the China Meteorological Administration (CMA-ARMN) since 1992.
I. Uno +6 more
core +1 more source

