Results 51 to 60 of about 5,076 (307)
Data include IPSLCM5A2 model outputs (netcdf) required to reproduce the figures shown in the manuscript, as well as two supplement data tables for (1) water flux details and (2) a compilation of Cenomanian-Turonian redox data from previous publications.
Ladant, Jean-Baptiste +5 more
core +1 more source
Observed trends and EC‐Earth3 climate model projections demonstrate expressive changes in the Southeast Atlantic Hydrographic Basin, Brazil. Significant increases in rainfall intensity and dry spell duration in the present climate are followed by projected amplification of extreme precipitation under future warming, particularly under the SSP5‐8.5 ...
Pedro Lucas Oliveira‐Santos +4 more
wiley +1 more source
Global warming has intensified drought impacts across most arid regions, altering surface energy partitioning and atmospheric boundary layer (ABL) development. Using 1979–2018 ERA‐Interim reanalysis data, we show that the long‐term mean boundary layer height (BLH) over global arid regions is approximately 841.8 m, nearly 200 m higher than over humid ...
Rong Wang +4 more
wiley +1 more source
Climate during the Late Cretaceous is characterized by a long-term cooling trend interrupted by several periods of increased warming. This study focuses on the terrestrial response to two rapid climate events just prior to the K-Pg boundary marked by the
Anna K. Lesko +2 more
doaj +1 more source
During the Holocene, most of the climatic variability in the tropics has manifested through changes in the precipitation regime. Although there is relatively a large amount of information on this climatic variability from the lowlands during this time ...
Yosahandy Vázquez-Molina +8 more
doaj +1 more source
Beyond ENSO: Temperature, Rainfall Variability and Emerging Climate Risks in Belize
This study analyses 50 years (1975–2024) of Belize's climate data to evaluate ENSO's influence. Results show negligible ENSO impact on rainfall but a moderate signal in nighttime dry‐season temperatures, with El Niño years 0.5°C–1.0°C warmer than La Niña years.
Martha Guzman, James Renwick
wiley +1 more source
The results reveal that thermal stress varies substantially across the four AP regions, with winter cold stress in Region I, year‐round heat stress in Region II, pronounced summer heat stress in Region III, and persistent strong to very strong heat stress from late spring to early autumn in Region IV.
Waheed Ullah +5 more
wiley +1 more source
Atmosphere-ocean interactions are particularly strong along the Chile-Peru coast and largely account for the extreme aridity of the Atacama Desert. Near the center of the driest part of this coastal desert, we found that the embayment Bahía Mejillones ...
LUC ORTLIEB +8 more
doaj
In this paper results of climate simulation in East-European Plain (EEP) by coupled climate models (which take part in project PMIP II (Paleoclimate Modeling Intercomparison Project)) are tested for different climatic periods (pre-industrial, Last ...
P. A. Morozova
doaj +1 more source
Climate Change Final Products and Research Notebook (Group 11)
The final project deliverables for the iSci 3A12 Climate Change Project for Group 11 including the Paleoclimatology Podcast, Paleoclimatology Extended Abstract and Paleoclimatology Final Presentation.
Tweedle, Adam +3 more
core +1 more source

