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Titlebook: Development and Evaluation of High Resolution Climate System Models; Rucong Yu,Tianjun Zhou,Guangqing Zhou Book 2016 Springer Science+Busi

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https://doi.org/10.1007/978-3-030-86826-0ute of Atmospheric Physics (IAP), Chinese Academy of Sciences (CAS), over 30 years have passed since the IAP’s AGCM was first designed in 1982, during which time the model has been continually developed.
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Der Umbau der Grounded-Theory-Methodologien of the monsoon–ENSO relationship are also assessed, and some evidence of how to improve ENSO simulation is presented. In addition to the metrics, the performance of the LASG/IAP decadal prediction system is also assessed.
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,Metrics for Gauging Model Performance Over the East Asian–Western Pacific Domain,n of the monsoon–ENSO relationship are also assessed, and some evidence of how to improve ENSO simulation is presented. In addition to the metrics, the performance of the LASG/IAP decadal prediction system is also assessed.
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Rucong Yu,Tianjun Zhou,Guangqing ZhouSummarizes the recent progress of China in the development of high resolution climate models.Explores how to establish a flexible multi-model ensemble modeling tool.Presents mertics for gauging model
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Andrey Ronzhin,Tien Ngo,Quyen Vu,Vinh Nguyenant No. 2010CB951900 is presented. The background and the objectives of the project are introduced. The main progress made in the past 5 years of the project is the development of “one system” and “two platforms”, where “one system” refers to the high-resolution modeling system and “two platforms” r
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https://doi.org/10.1007/978-3-030-86826-0tem model. The development of higher resolution AGCMs and OGCMs is one of the most active areas of study in the model development field. At the Institute of Atmospheric Physics (IAP), Chinese Academy of Sciences (CAS), over 30 years have passed since the IAP’s AGCM was first designed in 1982, during
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Andrey Ronzhin,Tien Ngo,Quyen Vu,Vinh Nguyens presented. It is an atmospheric and oceanic fully coupled climate model system with a horizontal resolution of T266 (approximately 45 × 45 km) in the atmosphere and 30 × 30 km in the tropical ocean. It was developed on the basis of a lower resolution version of the model (BCC_CSM1.1) [T42 (approxi
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