Historical and future extremes of cauvery basin analysed using cmip6 models and ETCCDI indices. [PDF]
Sridhara S +6 more
europepmc +1 more source
ERA5 Can Overstate Changes in the Frequency of Extreme Heat: A New Zealand Case Study
ERA5 reproduces broad patterns of summer warming across New Zealand but underestimates temperature variability and warm‐tail extremes, biasing estimates of extreme heat risk. ABSTRACT Summertime temperature extremes exert profound impacts on human health, ecosystems, and infrastructure, yet their characteristics and drivers remain poorly quantified in ...
Sayed Waseem Iqbal +2 more
wiley +1 more source
Assessing future landslide susceptibility and risk escalations under changing LULC and climate conditions in the Western Ghats of Karnataka in India. [PDF]
Pramanik M, Hegde A.
europepmc +1 more source
Annual and Seasonal Rainfall Variability in Mozambique During the Nineteenth Century
This paper presents the first annually and seasonally resolved reconstructions of nineteenth‐century rainfall variability for Mozambique derived from the analysis of extensive documentary evidence. It reveals spatially heterogeneous rainfall patterns with recurrent multi‐year droughts, episodic extreme wet events, and a strong coherence between ...
David J. Nash +2 more
wiley +1 more source
Observed and projected climate extremes in northwest highlands of Ethiopia and their implications in potato-based farming systems. [PDF]
Ayalew A +5 more
europepmc +1 more source
Four decades of UTCI data show increasing thermal stress along Ghana's coastal‐urban corridor, with very strong heat‐stress days rising by about 1.4 days/year. Random Forest–SHAP analysis with temporal validation identified AOD as the strongest model‐based predictor of monthly UTCI variability, followed by TSA, WHWP, and AMO.
Kwadwo Frimpong +3 more
wiley +1 more source
Deep vision-based framework for coastal flood prediction under sea level rise and shoreline protection. [PDF]
Karapetyan A, Chow ACH, Madanat S.
europepmc +1 more source
Climate Change Projections for Mexico in the 21st Century
Projected national temperature by the end of the century under four SSP scenarios. Under the low‐emission pathway (SSP1‐2.6), warming increases more gradually, whereas under the high‐emission scenario (SSP5‐8.5), temperatures exceed 5°C by 2100. These results strengthen the scientific basis for climate adaptation planning and long‐term decision‐making ...
Arhat Tejeda‐Aguilar +3 more
wiley +1 more source
Modeling the role of planting density and fertilizer in reducing the negative effects of rainfall variability on sorghum production in eastern Ethiopia using APSIM. [PDF]
Ebbisa AF +3 more
europepmc +1 more source

