Climatic and Hydrological Changes Drive Contemporary Fire Regime Transitions in the World's Largest Wetland. [PDF]
Barros-Rosa L +17 more
europepmc +1 more source
The changes in joint return period of compound meteorological hot‐dry (CMHHE) and hot‐wet (CMHWE) and compound hydrological hot‐dry (CHHDE) and hot‐wet (CHHWE) extremes were attributed to changes in associated univariate extremes and their dependence.
Ruting Yang +6 more
wiley +1 more source
Rainfall frequency and uncertainty analysis in arid regions using machine learning and statistical distribution models based on a 91-year rainfall record. [PDF]
Hagage M.
europepmc +1 more source
ENSO or the Atlantic: Which Actually Governs the Hydrological Vulnerability of the Caatinga?
This study challenges the traditional ENSO‐centric paradigm of rainfall variability in the Caatinga by demonstrating that the Tropical Atlantic exerts a statistically dominant influence on regional hydrological vulnerability. Using a seasonal ARX/HAC model and CHIRPS data, we establish a new hierarchy of climatic drivers across six rainfall districts ...
Jonathan Antunes Ponte Cavalcante Leite +3 more
wiley +1 more source
Assessing the onset of spring water-level rise in snowmelt-dominated rivers of northeastern Russia using machine learning. [PDF]
Malashin I +5 more
europepmc +1 more source
Sensitivity of Consecutive‐Dry‐Day Trends to Trace Loss in Matched Precipitation Archives
Loss of trace precipitation information can turn valid dry days into missing observations that interrupt consecutive dry day (CDD) spells. Simulating this loss reduced the median cross‐archive CDD trend discrepancy by 88% across 205 matched Spanish station pairs; a separate global experiment converting documented traces to missing observations changed ...
Marc Sempera +3 more
wiley +1 more source
Overcoming single model bias through GRACE and multi model data reveals Iran water storage depletion drivers. [PDF]
Yuan X, Wang F, Zhou Y, Zhou 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
Uncertainty analysis in the simulation of hydrological processes in Euphrates River Basin with contrasting climates. [PDF]
Al-Hammad SH +6 more
europepmc +1 more source

