To develop measures to reduce the vulnerability of forests drought, it is necessary estimate specific water balances in sites and their development with climate change scenarios. We quantified balance seven forest monitoring northeast Germany for historical time period 1961–2019, projections 2010–2100. used LWF-BROOK90 hydrological model forced data, bias-adjusted data from two models fifth pha...

The Pacific region of Colombia is known to be one the most vulnerable changes in precipitation patterns. A study was conducted using standardized index (SPI) analyses understand potential this during 21st century. were historical data from 1950 2005 and projected 2022 2100 under Coordinated Regional Climate Downscaling Experiment (CORDEX) climate scenarios (RCP 4.5 RCP 8.5). results showed that...

Abstract Quantifying the impact of climate change on evapotranspiration is necessary for devising accurate water and energy budgets in light global warming. Nevertheless, Middle East North Africa (MENA), little has been done to bridge this gap. This study, then, implements Penman Budyko approaches climatic data retrieved from sixth phase Coupled Model Intercomparison Project (CMIP6) assess avai...

Brown spot needle blight (BSNB), caused by Lecanosticta acicola (Thüm.) Syd., is an emerging forest disease of Pinus species originating from North America and introduced to Europe Asia. Severity spread the has increased in last two decades as a response climate change. No modeling work on spread, severity, climatic suitability, or potential distribution been done for this important pathogen. T...

For future climate projections to be useful they must actionable at the local level. In this study, we develop daily temperature and precipitation scenarios suitable for use in of drought, energy use, water crop production. We investigate magnitude changes air Midwest United States response three change scenarios. Results are used assess incidence extremes human comfort (using heat index) assoc...

Atmospheric carbon dioxide (CO2) would be increasing much more if it were not for terrestrial (C) uptake, fueling the drawdown of atmospheric CO2 in vegetation and soil on decadal to centennial time scales. Here, we used a global Earth system model (BNU-ESM) with two different data sets (i.e., uniform vs. non-uniform sets) simulate responses C balance, particularly effect. Under future conditio...