Zobrazeno 1 - 10
of 86
pro vyhledávání: '"M. Kawamiya"'
Publikováno v:
Geoscientific Model Development, Vol 14, Pp 1195-1217 (2021)
Following the protocol of the fourth phase of the Paleoclimate Modelling Intercomparison Project (PMIP4), we performed numerical experiments targeting distinctive past time periods using the Model for Interdisciplinary Research on Climate, Earth Syst
Externí odkaz:
https://doaj.org/article/9f4d2d42d1274adca0b3f84267f296b1
Publikováno v:
Ocean Science, Vol 16, Pp 1431-1442 (2020)
Based on a set of climate simulations utilizing two kinds of Earth system models (ESMs) in which observed ocean hydrographic data are assimilated using exactly the same data assimilation procedure, we have clarified that the successful simulation of
Externí odkaz:
https://doaj.org/article/d9de9772970b43bfb02216f17fb746d9
Autor:
V. K. Arora, A. Katavouta, R. G. Williams, C. D. Jones, V. Brovkin, P. Friedlingstein, J. Schwinger, L. Bopp, O. Boucher, P. Cadule, M. A. Chamberlain, J. R. Christian, C. Delire, R. A. Fisher, T. Hajima, T. Ilyina, E. Joetzjer, M. Kawamiya, C. D. Koven, J. P. Krasting, R. M. Law, D. M. Lawrence, A. Lenton, K. Lindsay, J. Pongratz, T. Raddatz, R. Séférian, K. Tachiiri, J. F. Tjiputra, A. Wiltshire, T. Wu, T. Ziehn
Publikováno v:
Biogeosciences, Vol 17, Pp 4173-4222 (2020)
Results from the fully and biogeochemically coupled simulations in which CO2 increases at a rate of 1 % yr−1 (1pctCO2) from its preindustrial value are analyzed to quantify the magnitude of carbon–concentration and carbon–climate feedback p
Externí odkaz:
https://doaj.org/article/94990c91dee946e5b96eace492047b42
Autor:
T. Hajima, M. Watanabe, A. Yamamoto, H. Tatebe, M. A. Noguchi, M. Abe, R. Ohgaito, A. Ito, D. Yamazaki, H. Okajima, K. Takata, K. Ogochi, S. Watanabe, M. Kawamiya
Publikováno v:
Geoscientific Model Development, Vol 13, Pp 2197-2244 (2020)
This article describes the new Earth system model (ESM), the Model for Interdisciplinary Research on Climate, Earth System version 2 for Long-term simulations (MIROC-ES2L), using a state-of-the-art climate model as the physical core. This model embed
Externí odkaz:
https://doaj.org/article/bab0cf94cb1f4da0b2a4687792bbdeee
Autor:
R. Ohgaito, A. Abe-Ouchi, R. O'ishi, T. Takemura, A. Ito, T. Hajima, S. Watanabe, M. Kawamiya
Publikováno v:
Climate of the Past, Vol 14, Pp 1565-1581 (2018)
The effect of aerosols is one of many uncertain factors in projections of future climate. However, the behaviour of mineral dust aerosols (dust) can be investigated within the context of past climate change. The Last Glacial Maximum (LGM) is known
Externí odkaz:
https://doaj.org/article/300a6ee6d7de4a008fe9d06fc4716af3
Autor:
C. D. Jones, V. Arora, P. Friedlingstein, L. Bopp, V. Brovkin, J. Dunne, H. Graven, F. Hoffman, T. Ilyina, J. G. John, M. Jung, M. Kawamiya, C. Koven, J. Pongratz, T. Raddatz, J. T. Randerson, S. Zaehle
Publikováno v:
Geoscientific Model Development, Vol 9, Iss 8, Pp 2853-2880 (2016)
Coordinated experimental design and implementation has become a cornerstone of global climate modelling. Model Intercomparison Projects (MIPs) enable systematic and robust analysis of results across many models, by reducing the influence of ad hoc di
Externí odkaz:
https://doaj.org/article/b43904a5112f469ba42902eb5e34e766
Autor:
R. Ohgaito, T. Sueyoshi, A. Abe-Ouchi, T. Hajima, S. Watanabe, H.-J. Kim, A. Yamamoto, M. Kawamiya
Publikováno v:
Climate of the Past, Vol 9, Iss 4, Pp 1519-1542 (2013)
The importance of evaluating models through paleoclimate simulations is becoming more recognized in efforts to improve climate projection. To evaluate an integrated Earth System Model, MIROC-ESM, we performed simulations in time-slice experiments for
Externí odkaz:
https://doaj.org/article/c211b168762e458ca4dc5cab50cbc143
Autor:
T. Sueyoshi, R. Ohgaito, A. Yamamoto, M. O. Chikamoto, T. Hajima, H. Okajima, M. Yoshimori, M. Abe, R. O'ishi, F. Saito, S. Watanabe, M. Kawamiya, A. Abe-Ouchi
Publikováno v:
Geoscientific Model Development, Vol 6, Iss 3, Pp 819-836 (2013)
Paleoclimate experiments using contemporary climate models are an effective measure to evaluate climate models. In recent years, Earth system models (ESMs) were developed to investigate carbon cycle climate feedbacks, as well as to project the future
Externí odkaz:
https://doaj.org/article/c9078f85c2d94c90aeb9e41ab7b305bf
Autor:
M. Eby, A. J. Weaver, K. Alexander, K. Zickfeld, A. Abe-Ouchi, A. A. Cimatoribus, E. Crespin, S. S. Drijfhout, N. R. Edwards, A. V. Eliseev, G. Feulner, T. Fichefet, C. E. Forest, H. Goosse, P. B. Holden, F. Joos, M. Kawamiya, D. Kicklighter, H. Kienert, K. Matsumoto, I. I. Mokhov, E. Monier, S. M. Olsen, J. O. P. Pedersen, M. Perrette, G. Philippon-Berthier, A. Ridgwell, A. Schlosser, T. Schneider von Deimling, G. Shaffer, R. S. Smith, R. Spahni, A. P. Sokolov, M. Steinacher, K. Tachiiri, K. Tokos, M. Yoshimori, N. Zeng, F. Zhao
Publikováno v:
Climate of the Past, Vol 9, Iss 3, Pp 1111-1140 (2013)
Both historical and idealized climate model experiments are performed with a variety of Earth system models of intermediate complexity (EMICs) as part of a community contribution to the Intergovernmental Panel on Climate Change Fifth Assessment Repor
Externí odkaz:
https://doaj.org/article/50618918886b4d02a97e242bffe2bdcb
Publikováno v:
Biogeosciences, Vol 9, Iss 6, Pp 2365-2375 (2012)
The largest pH decline and widespread undersaturation with respect to aragonite in this century due to uptake of anthropogenic carbon dioxide in the Arctic Ocean have been projected. The reductions in pH and aragonite saturation state in the Arctic O
Externí odkaz:
https://doaj.org/article/f4b5e6299fd440cca4fa5a3775ae100b