Auswahl der wissenschaftlichen Literatur zum Thema „IPSL-CM6A-LR“
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Zeitschriftenartikel zum Thema "IPSL-CM6A-LR"
Din, Salah Ud. „Flow prediction in Kabul River: An artificial intelligence based technique“. International Journal of Multidisciplinary Research and Growth Evaluation 5, Nr. 2 (2024): 854–57. http://dx.doi.org/10.54660/.ijmrge.2024.5.2.854-857.
Der volle Inhalt der QuelleAndrade-Velázquez, Mercedes, und Martín José Montero-Martínez. „Statistical Downscaling of Precipitation in the South and Southeast of Mexico“. Climate 11, Nr. 9 (08.09.2023): 186. http://dx.doi.org/10.3390/cli11090186.
Der volle Inhalt der QuellePoletti, Alyssa N., Dargan M. W. Frierson, Travis Aerenson, Akshaya Nikumbh, Rachel Carroll, William Henshaw und Jack Scheff. „Atmosphere and ocean energy transport in extreme warming scenarios“. PLOS Climate 3, Nr. 2 (01.02.2024): e0000343. http://dx.doi.org/10.1371/journal.pclm.0000343.
Der volle Inhalt der QuelleÜyük, Ayyüce, und Ömer K. Örücü. „Platanus orientalis L. (Doğu Çınarı) günümüz ve gelecek yayılış alanlarının CanESM5ve IPSL-CM6A-LR iklim modellerine göre karşılaştırılması“. Ecological Perspective 2, Nr. 1 (06.07.2022): 137–50. http://dx.doi.org/10.53463/ecopers.20220146.
Der volle Inhalt der QuelleSarikaya, Ayse Gul, und Almira Uzun. „Modeling the Effects of Climate Change on the Current and Future Potential Distribution of Berberis vulgaris L. with Machine Learning“. Sustainability 16, Nr. 3 (01.02.2024): 1230. http://dx.doi.org/10.3390/su16031230.
Der volle Inhalt der QuelleXiao, Heng, Yue Zhuo, Hong Sun, Kaiwen Pang und Zhijia An. „Evaluation and Projection of Climate Change in the Second Songhua River Basin Using CMIP6 Model Simulations“. Atmosphere 14, Nr. 9 (12.09.2023): 1429. http://dx.doi.org/10.3390/atmos14091429.
Der volle Inhalt der QuelleRaila, Shiva Nath, Raju Acharya, Sudan Ghimire, Subash Adhikari, Saroj Khanal, Yogendra Mishra und Manoj Lamichhane. „Out-Performing Bias-Corrected GCM Models and CMIP6-Based Precipitation and Temperature Projections for the Bagmati Irrigation Area“. Journal of Advanced College of Engineering and Management 7, Nr. 01 (25.08.2022): 165–72. http://dx.doi.org/10.3126/jacem.v7i01.47342.
Der volle Inhalt der QuelleBabaousmail, Hassen, Rongtao Hou, Brian Ayugi, Moses Ojara, Hamida Ngoma, Rizwan Karim, Adharsh Rajasekar und Victor Ongoma. „Evaluation of the Performance of CMIP6 Models in Reproducing Rainfall Patterns over North Africa“. Atmosphere 12, Nr. 4 (09.04.2021): 475. http://dx.doi.org/10.3390/atmos12040475.
Der volle Inhalt der QuelleSmith, Christopher J., Ryan J. Kramer und Adriana Sima. „The HadGEM3-GA7.1 radiative kernel: the importance of a well-resolved stratosphere“. Earth System Science Data 12, Nr. 3 (13.09.2020): 2157–68. http://dx.doi.org/10.5194/essd-12-2157-2020.
Der volle Inhalt der QuelleRagab, Sanad H., und Michael G. Tyshenko. „Predicting the potential worldwide distribution of Aedes aegypti under climate change scenarios“. International Journal of Scientific Reports 9, Nr. 11 (23.10.2023): 344–52. http://dx.doi.org/10.18203/issn.2454-2156.intjscirep20233163.
Der volle Inhalt der QuelleDissertationen zum Thema "IPSL-CM6A-LR"
Feng, Yang. „Study of the climate variability and the role of volcanism in the North Atlantic-Mediterranean sector during the last millennium“. Electronic Thesis or Diss., Sorbonne université, 2022. http://www.theses.fr/2022SORUS038.
Der volle Inhalt der QuelleThe PhD work aims at studying the role of volcanism in influencing winter climate variability (especially, NAO) over the North Atlantic-Mediterranean sector at inter-annual scale. The first part is devoted to characterizing the simulated NAO signal in winters following stratospheric volcanic eruptions using three long transient simulations of the past millennium (500-1849 CE) by IPSL-CM6A-LR in the frame of PMIP4. The robustness and sensitivity of the response related to the latitude, season and strength of the eruptions are also explored. The second part extends further to decrypt the physical mechanism regarding different components of volcanic radiative forcing (the surface cooling and stratospheric warming). The work focuses on three 25-members ensemble simulations by IPSL-CM6A-LR following the VolMIP protocol for the well observed Mt. Pinatubo tropical eruption (Philippines, June 1991). Sensitivity experiments indicate that the surface positive NAO signature in our model experiments is primarily attributable to heating in the lower tropical stratosphere which generates stronger subtropical zonal winds through the thermal wind balance and accelerates the polar vortex. Stationary planetary wave propagations are also playing indispensable modulations effects