Results 41 to 50 of about 24,239 (287)

Bias correction and projection of temperature over the altitudes of the Upper Indus Basin under CMIP6 climate scenarios from 1985 to 2100

Journal of Water and Climate Change, 2023
The identification of projected changes in temperature caused by global warming at a fine-scale spatial resolution is of great importance for the high-altitude glacier and snow covered Upper Indus Basin.
Kashif Jamal, Xin Li, Yingying Chen, Muhammad Rizwan, Muhammad Adnan Khan, Zain Syed, Prince Mahmood   +6 more
doaj   +1 more source

Requirements for a global data infrastructure in support of CMIP6 [PDF]

, 2018
The World Climate Research Programme (WCRP)’s Working Group on Climate Modelling (WGCM) Infrastructure Panel (WIP) was formed in 2014 in response to the explosive growth in size and complexity of Coupled Model Intercomparison Projects (CMIPs) between ...
A. Radhakrishnan, A. Radhakrishnan, B. N. Lawrence, B. N. Lawrence, C. Blanton, C. Blanton, D. Hassell, D. Williams, E. Guilyardi, E. Guilyardi, F. Guglielmo, K. E. Taylor, L. Cinquini, M. Elkington, M. Juckes, M. Lautenschlager, M. Stockhause, P. J. Durack, S. Denvil, S. Kharin, S. Kindermann, S. Nikonov, S. Nikonov, T. Weigel, V. Balaji, V. Balaji   +25 more
core   +4 more sources

Evaluation of CMIP6 models in reproducing observed rainfall over Ethiopia

Journal of Water and Climate Change, 2023
Ethiopia is highly susceptible to the effects of climate change and variability. This study evaluated the performances of 37 CMIP6 models against a gridded rainfall product of Ethiopia known as Enhancing National Climate Services (ENACTS) in simulating ...
Daniel Berhanu, Tena Alamirew, Meron Teferi Taye, Degefie Tibebe, Solomon Gebrehiwot, Gete Zeleke   +5 more
doaj   +1 more source

Historical and Projected Surface Temperature over India during the 20th and 21st century. [PDF]

, 2017
Surface Temperature (ST) over India has increased by ~0.055 K/decade during 1860-2005 and follows the global warming trend. Here, the natural and external forcings (e.g., natural and anthropogenic) responsible for ST variability are studied from Coupled ...
Agha Kouchak, Amir, Basha, Ghouse, Jayaraman, A, Kishore, P, Ouarda, Taha BMJ, Ratnam, M Venkat, Velicogna, Isabella   +6 more
core   +2 more sources

Assessment of climate change impacts on hydrological processes in the Usangu catchment of Tanzania under CMIP6 scenarios

Journal of Water and Climate Change, 2023
Climate change is anticipated to have long-term effects on hydrological processes and patterns, leading to water stress in agroecological catchments. Climate change escalates water scarcity in the Usangu catchment, as evidenced by the drying up of rivers
Gift Raphael Mollel, Deogratias M. M. Mulungu, Joel Nobert, Augustina C. Alexander   +3 more
doaj   +1 more source

Regional-scale flood impacts on a small mountainous catchment in Thailand under a changing climate

Journal of Water and Climate Change, 2023
Extreme rainfall and flooding are common during the summer monsoon season in Thailand. In this study, we utilized Robust Empirical Quantile Mapping (RQUANT) to correct the bias in precipitation, and total runoff data obtained from the latest Couple Model
Sawitree Rojpratak, Seree Supharatid
doaj   +1 more source

CMIP6 climate models imply high committed warming [PDF]

Climatic Change, 2020
This is the final version. Available from the publisher via the DOI in this record. ; Data availability The CO2e time series is from the RCP scenario site, selecting the rcp85 file: http://www.pikpotsdam.de/~mmalte/rcps/.
Chris Huntingford, Mark S. Williamson, Femke J. M. M. Nijsse   +2 more
openaire   +4 more sources

Mathematical modeling of Elbrus glaciers in the 21st century. Part 2. Forecasting glacier evolution and lake formation under various SSP scenarios

Лëд и снег
Probable scenarios of future changes in the Elbrus glaciers and associated with them phenomena such as formation of glacial lakes and remaining ice masses buried under the debris cover are considered. The SSP scenarios (SSP1–1.9, SSP1–2.6, SSP2–4.5, SSP3–
T. N. Postnikova, O. O. Rybak, A. S. Gubanov, H. Zekollari, M. Huss   +4 more
doaj   +1 more source

Performance analysis of individual climate models for evapotranspiration projections over Hatay Province [PDF]

Aerul şi Apa: Componente ale Mediului
Evapotranspiration, one of the basic components of hydrology, can cause significant decreases in water levels. Especially in regions sensitive to climate change, evapotranspiration is of critical importance in terms of water structures planning and water
Fatih ÜNEŞ, Yunus Ziya KAYA, Samed GÖÇMEN   +2 more
doaj   +1 more source

qhgogogo/CMIP6-carbonflux:

, 2021
codes for the CMIP6 cabron fluxes ...
openaire   +1 more source