Zobrazeno 1 - 10
of 139
pro vyhledávání: '"F. Paulot"'
Publikováno v:
Atmospheric Chemistry and Physics, Vol 24, Pp 4217-4229 (2024)
Hydrogen (H2) is a promising low-carbon alternative to fossil fuels for many applications. However, significant gaps in our understanding of the atmospheric H2 budget limit our ability to predict the impacts of greater H2 usage. Here we use NOAA H2 d
Externí odkaz:
https://doaj.org/article/328b182a5c1549c7aa9395cae7f8eae2
Autor:
W. Tang, B. B. Ward, M. Beman, L. Bristow, D. Clark, S. Fawcett, C. Frey, F. Fripiat, G. J. Herndl, M. Mdutyana, F. Paulot, X. Peng, A. E. Santoro, T. Shiozaki, E. Sintes, C. Stock, X. Sun, X. S. Wan, M. N. Xu, Y. Zhang
Publikováno v:
Earth System Science Data, Vol 15, Pp 5039-5077 (2023)
As a key biogeochemical pathway in the marine nitrogen cycle, nitrification (ammonia oxidation and nitrite oxidation) converts the most reduced form of nitrogen – ammonium–ammonia (NH4+–NH3) – into the oxidized species nitrite (NO2-) and nitr
Externí odkaz:
https://doaj.org/article/6baf8a77ab074f20a0d42e1ef93eba46
Autor:
J. Quaas, H. Jia, C. Smith, A. L. Albright, W. Aas, N. Bellouin, O. Boucher, M. Doutriaux-Boucher, P. M. Forster, D. Grosvenor, S. Jenkins, Z. Klimont, N. G. Loeb, X. Ma, V. Naik, F. Paulot, P. Stier, M. Wild, G. Myhre, M. Schulz
Publikováno v:
Atmospheric Chemistry and Physics, Vol 22, Pp 12221-12239 (2022)
Anthropogenic aerosols exert a cooling influence that offsets part of the greenhouse gas warming. Due to their short tropospheric lifetime of only several days, the aerosol forcing responds quickly to emissions. Here, we present and discuss the evolu
Externí odkaz:
https://doaj.org/article/dbe19c76e213429d9f0ed51c189f1b57
Publikováno v:
AGU Advances, Vol 3, Iss 6, Pp n/a-n/a (2022)
Abstract Bubbles bursting at the ocean surface are an important source of ocean‐spray aerosol, with implications on radiative and cloud processes. Yet, very large uncertainties exist on the role of key physical controlling parameters, including win
Externí odkaz:
https://doaj.org/article/59eaaff5dfc64042a28a90afb06e7c73
Autor:
G. Thornhill, W. Collins, D. Olivié, R. B. Skeie, A. Archibald, S. Bauer, R. Checa-Garcia, S. Fiedler, G. Folberth, A. Gjermundsen, L. Horowitz, J.-F. Lamarque, M. Michou, J. Mulcahy, P. Nabat, V. Naik, F. M. O'Connor, F. Paulot, M. Schulz, C. E. Scott, R. Séférian, C. Smith, T. Takemura, S. Tilmes, K. Tsigaridis, J. Weber
Publikováno v:
Atmospheric Chemistry and Physics, Vol 21, Pp 1105-1126 (2021)
Feedbacks play a fundamental role in determining the magnitude of the response of the climate system to external forcing, such as from anthropogenic emissions. The latest generation of Earth system models includes aerosol and chemistry components tha
Externí odkaz:
https://doaj.org/article/13a27c7c269d4e36a79f7adbb3f3cc95
Autor:
L. Kuai, K. W. Bowman, K. Miyazaki, M. Deushi, L. Revell, E. Rozanov, F. Paulot, S. Strode, A. Conley, J.-F. Lamarque, P. Jöckel, D. A. Plummer, L. D. Oman, H. Worden, S. Kulawik, D. Paynter, A. Stenke, M. Kunze
Publikováno v:
Atmospheric Chemistry and Physics, Vol 20, Pp 281-301 (2020)
The top-of-atmosphere (TOA) outgoing longwave flux over the 9.6 µm ozone band is a fundamental quantity for understanding chemistry–climate coupling. However, observed TOA fluxes are hard to estimate as they exhibit considerable variability in s
Externí odkaz:
https://doaj.org/article/1c86cd4e6a034aed9bc1893ed60d400e
Autor:
I. M. Held, H. Guo, A. Adcroft, J. P. Dunne, L. W. Horowitz, J. Krasting, E. Shevliakova, M. Winton, M. Zhao, M. Bushuk, A. T. Wittenberg, B. Wyman, B. Xiang, R. Zhang, W. Anderson, V. Balaji, L. Donner, K. Dunne, J. Durachta, P. P. G. Gauthier, P. Ginoux, J.‐C. Golaz, S. M. Griffies, R. Hallberg, L. Harris, M. Harrison, W. Hurlin, J. John, P. Lin, S.‐J. Lin, S. Malyshev, R. Menzel, P. C. D. Milly, Y. Ming, V. Naik, D. Paynter, F. Paulot, V. Ramaswamy, B. Reichl, T. Robinson, A. Rosati, C. Seman, L. G. Silvers, S. Underwood, N. Zadeh
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 11, Iss 11, Pp 3691-3727 (2019)
Abstract We describe the Geophysical Fluid Dynamics Laboratory's CM4.0 physical climate model, with emphasis on those aspects that may be of particular importance to users of this model and its simulations. The model is built with the AM4.0/LM4.0 atm
Externí odkaz:
https://doaj.org/article/2783ed629b8548859de4589a835f3983
Publikováno v:
Atmospheric Chemistry and Physics, Vol 18, Pp 17963-17978 (2018)
Reactive nitrogen (N) emissions have increased over the last 150 years as a result of greater fossil fuel combustion and food production. The resulting increase in N deposition can alter the function of ecosystems, but characterizing its ecologica
Externí odkaz:
https://doaj.org/article/43bc99af1d16466d9d2f50484d0e6642
Autor:
J. P. Dunne, L. W. Horowitz, A. J. Adcroft, P. Ginoux, I. M. Held, J. G. John, J. P. Krasting, S. Malyshev, V. Naik, F. Paulot, E. Shevliakova, C. A. Stock, N. Zadeh, V. Balaji, C. Blanton, K. A. Dunne, C. Dupuis, J. Durachta, R. Dussin, P. P. G. Gauthier, S. M. Griffies, H. Guo, R. W. Hallberg, M. Harrison, J. He, W. Hurlin, C. McHugh, R. Menzel, P. C. D. Milly, S. Nikonov, D. J. Paynter, J. Ploshay, A. Radhakrishnan, K. Rand, B. G. Reichl, T. Robinson, D. M. Schwarzkopf, L. T. Sentman, S. Underwood, H. Vahlenkamp, M. Winton, A. T. Wittenberg, B. Wyman, Y. Zeng, M. Zhao
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 12, Iss 11, Pp n/a-n/a (2020)
Abstract We describe the baseline coupled model configuration and simulation characteristics of GFDL's Earth System Model Version 4.1 (ESM4.1), which builds on component and coupled model developments at GFDL over 2013–2018 for coupled carbon‐che
Externí odkaz:
https://doaj.org/article/2d282ef73bac47f3943c7760f0275b10
Publikováno v:
Atmospheric Chemistry and Physics, Vol 18, Pp 13265-13281 (2018)
We present estimates of changes in the direct aerosol effects (DRE) and its anthropogenic component (DRF) from 2001 to 2015 using the GFDL chemistry–climate model AM3 driven by CMIP6 historical emissions. AM3 is evaluated against observed change
Externí odkaz:
https://doaj.org/article/8f8ca37f30f84768b28f767658af2a1d