Zobrazeno 1 - 10
of 14
pro vyhledávání: '"I. R. Simpson"'
Autor:
B. M. Sanderson, B. B. B. Booth, J. Dunne, V. Eyring, R. A. Fisher, P. Friedlingstein, M. J. Gidden, T. Hajima, C. D. Jones, C. G. Jones, A. King, C. D. Koven, D. M. Lawrence, J. Lowe, N. Mengis, G. P. Peters, J. Rogelj, C. Smith, A. C. Snyder, I. R. Simpson, A. L. S. Swann, C. Tebaldi, T. Ilyina, C.-F. Schleussner, R. Séférian, B. H. Samset, D. van Vuuren, S. Zaehle
Publikováno v:
Geoscientific Model Development, Vol 17, Pp 8141-8172 (2024)
Previous phases of the Coupled Model Intercomparison Project (CMIP) have primarily focused on simulations driven by atmospheric concentrations of greenhouse gases (GHGs), for both idealized model experiments and climate projections of different emiss
Externí odkaz:
https://doaj.org/article/17490fbda0b743d99824e7d3ac5584c8
Autor:
M. M. Holland, C. Hannay, J. Fasullo, A. Jahn, J. E. Kay, M. Mills, I. R. Simpson, W. Wieder, P. Lawrence, E. Kluzek, D. Bailey
Publikováno v:
Geoscientific Model Development, Vol 17, Pp 1585-1602 (2024)
Climate simulation uncertainties arise from internal variability, model structure, and external forcings. Model intercomparisons (such as the Coupled Model Intercomparison Project; CMIP) and single-model large ensembles have provided insight into unc
Externí odkaz:
https://doaj.org/article/6f273a2c3d624040a494124e7bccacc6
Publikováno v:
Weather and Climate Dynamics, Vol 4, Pp 853-874 (2023)
It has been demonstrated that decadal variations in the North Atlantic Oscillation (NAO) can be predicted by current forecast models. While Atlantic Multidecadal Variability (AMV) in sea surface temperatures (SSTs) has been hypothesised as the source
Externí odkaz:
https://doaj.org/article/0858aab40b78466bbe8b1b876da398b0
Autor:
P. Hitchcock, A. Butler, A. Charlton-Perez, C. I. Garfinkel, T. Stockdale, J. Anstey, D. Mitchell, D. I. V. Domeisen, T. Wu, Y. Lu, D. Mastrangelo, P. Malguzzi, H. Lin, R. Muncaster, B. Merryfield, M. Sigmond, B. Xiang, L. Jia, Y.-K. Hyun, J. Oh, D. Specq, I. R. Simpson, J. H. Richter, C. Barton, J. Knight, E.-P. Lim, H. Hendon
Publikováno v:
Geoscientific Model Development, Vol 15, Pp 5073-5092 (2022)
Major disruptions of the winter season, high-latitude stratospheric polar vortices can result in stratospheric anomalies that persist for months. These sudden stratospheric warming events are recognized as an important potential source of forecast sk
Externí odkaz:
https://doaj.org/article/b5ebaa5dcc3440ee83b37563b352c396
Publikováno v:
Atmospheric Chemistry and Physics, Vol 22, Pp 197-214 (2022)
Specified dynamics schemes are ubiquitous modeling tools for isolating the roles of dynamics and transport on chemical weather and climate. They typically constrain the circulation of a chemistry–climate model to the circulation in a reanalysis pro
Externí odkaz:
https://doaj.org/article/1837f610f016460ea59ca66936b0882f
Autor:
K. B. Rodgers, S.-S. Lee, N. Rosenbloom, A. Timmermann, G. Danabasoglu, C. Deser, J. Edwards, J.-E. Kim, I. R. Simpson, K. Stein, M. F. Stuecker, R. Yamaguchi, T. Bódai, E.-S. Chung, L. Huang, W. M. Kim, J.-F. Lamarque, D. L. Lombardozzi, W. R. Wieder, S. G. Yeager
Publikováno v:
Earth System Dynamics, Vol 12, Pp 1393-1411 (2021)
While climate change mitigation targets necessarily concern maximum mean state changes, understanding impacts and developing adaptation strategies will be largely contingent on how climate variability responds to increasing anthropogenic perturbation
Externí odkaz:
https://doaj.org/article/7856af5748394191b14fd012b3355da0
Publikováno v:
Atmospheric Chemistry and Physics, Vol 21, Pp 6985-6997 (2021)
It has been suggested that increased stratospheric sulfate aerosol loadings following large, low latitude volcanic eruptions can lead to wintertime warming over Eurasia through dynamical stratosphere–troposphere coupling. We here investigate the pr
Externí odkaz:
https://doaj.org/article/d827b7b61bd24631bd4df0837c1d18b7
Autor:
A. Gettelman, J. E. Truesdale, J. T. Bacmeister, P. M. Caldwell, R. B. Neale, P. A. Bogenschutz, I. R. Simpson
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 11, Iss 5, Pp 1381-1401 (2019)
Abstract The Single Column Atmosphere Model (SCAM) is a single column model version of the Community Atmosphere Model (CAM). Here we describe the functionality and features of SCAM6, available as part of CAM6 in the Community Earth System Model, vers
Externí odkaz:
https://doaj.org/article/0c642d8f451b4767a3caa3f71982be41
Autor:
O. Adam, K. M. Grise, P. Staten, I. R. Simpson, S. M. Davis, N. A. Davis, D. W. Waugh, T. Birner, A. Ming
Publikováno v:
Geoscientific Model Development, Vol 11, Pp 4339-4357 (2018)
Observational and modeling studies suggest that Earth's tropical belt has widened over the late 20th century and will continue to widen throughout the 21st century. Yet, estimates of tropical-width variations differ significantly across studies. T
Externí odkaz:
https://doaj.org/article/3d8a0d58b32b4c54a2e089a253e6a7a7
Autor:
F. Serva, J. A. Anstey, A. C. Bushell, N. Butchart, C. Cagnazzo, L. J. Gray, Y. Kawatani, S. M. Osprey, J. H. Richter, I. R. Simpson
The processes occurring in the tropical tropopause layer (TTL) are of great importance for stratosphere–troposphere exchanges and the variability of the Earth's climate. Previous studies demonstrated the increasing ability of atmospheric general ci
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f9a0e9b9f4b7d01e1467049274a707ca
https://doi.org/10.1002/qj.4287
https://doi.org/10.1002/qj.4287
