Zobrazeno 1 - 10
of 465 769
pro vyhledávání: '"A. Ito"'
Autor:
H. Tian, N. Pan, R. L. Thompson, J. G. Canadell, P. Suntharalingam, P. Regnier, E. A. Davidson, M. Prather, P. Ciais, M. Muntean, S. Pan, W. Winiwarter, S. Zaehle, F. Zhou, R. B. Jackson, H. W. Bange, S. Berthet, Z. Bian, D. Bianchi, A. F. Bouwman, E. T. Buitenhuis, G. Dutton, M. Hu, A. Ito, A. K. Jain, A. Jeltsch-Thömmes, F. Joos, S. Kou-Giesbrecht, P. B. Krummel, X. Lan, A. Landolfi, R. Lauerwald, Y. Li, C. Lu, T. Maavara, M. Manizza, D. B. Millet, J. Mühle, P. K. Patra, G. P. Peters, X. Qin, P. Raymond, L. Resplandy, J. A. Rosentreter, H. Shi, Q. Sun, D. Tonina, F. N. Tubiello, G. R. van der Werf, N. Vuichard, J. Wang, K. C. Wells, L. M. Western, C. Wilson, J. Yang, Y. Yao, Y. You, Q. Zhu
Publikováno v:
Earth System Science Data, Vol 16, Pp 2543-2604 (2024)
Nitrous oxide (N2O) is a long-lived potent greenhouse gas and stratospheric ozone-depleting substance that has been accumulating in the atmosphere since the preindustrial period. The mole fraction of atmospheric N2O has increased by nearly 25 % from
Externí odkaz:
https://doaj.org/article/b9208774a5d14859ad61fa0fc132957a
Publikováno v:
Atmospheric Chemistry and Physics, Vol 24, Pp 1777-1799 (2024)
We investigated the association of marine biological indicators (polysaccharides, protein-like gel particles, and chl a) with the formation of fluorescent aerosol particles, cloud condensation nuclei (CCNs), and ice-nucleating particles (INPs) over t
Externí odkaz:
https://doaj.org/article/b9216472ef654c0a8b7f5ba37bb4caa8
Publikováno v:
Atmospheric Chemistry and Physics, Vol 23, Pp 14609-14626 (2023)
Trace metals in aerosol particles impact Earth's radiative budget, human health, and ocean biogeochemistry. Semi-continuous measurements of the elemental composition of fine-mode (PM2.5) aerosols were conducted using an automated X-ray fluorescence a
Externí odkaz:
https://doaj.org/article/014feeacad33492288922670f7628ee8
Publikováno v:
Atmospheric Measurement Techniques, Vol 17, Pp 165-166 (2024)
Externí odkaz:
https://doaj.org/article/fa08fe81bd6342e480e8f0c49f1c11b2
Autor:
A. Ito, T. Li, Z. Qin, J. R. Melton, H. Tian, T. Kleinen, W. Zhang, Z. Zhang, F. Joos, P. Ciais, P. O. Hopcroft, D. J. Beerling, X. Liu, Q. Zhuang, Q. Zhu, C. Peng, K.‐Y. Chang, E. Fluet‐Chouinard, G. McNicol, P. Patra, B. Poulter, S. Sitch, W. Riley
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 14, Pp n/a-n/a (2023)
Abstract Cold‐season methane (CH4) emissions may be poorly constrained in wetland models. We examined cold‐season CH4 emissions simulated by 16 models participating in the Global Carbon Project model intercomparison and analyzed temporal and spat
Externí odkaz:
https://doaj.org/article/e86c4d725ba545e596704381388736e2
Autor:
N. Chandra, P. K. Patra, Y. Niwa, A. Ito, Y. Iida, D. Goto, S. Morimoto, M. Kondo, M. Takigawa, T. Hajima, M. Watanabe
Publikováno v:
Atmospheric Chemistry and Physics, Vol 22, Pp 9215-9243 (2022)
Global and regional sources and sinks of carbon across the earth's surface have been studied extensively using atmospheric carbon dioxide (CO2) observations and atmospheric chemistry-transport model (ACTM) simulations (top-down/inversion method). How
Externí odkaz:
https://doaj.org/article/e8da8dfe365a439cad680ce9def2fdb6
Publikováno v:
Atmospheric Chemistry and Physics, Vol 22, Pp 6045-6066 (2022)
Mineral dust is the largest source of aerosol iron (Fe) to the offshore global ocean, but acidic processing of coal fly ash (CFA) in the atmosphere could be an important source of soluble aerosol Fe. Here, we determined the Fe speciation and dissolut
Externí odkaz:
https://doaj.org/article/19e71081aa58489ebc91ee613b2afc2f
Autor:
S. Myriokefalitakis, E. Bergas-Massó, M. Gonçalves-Ageitos, C. Pérez García-Pando, T. van Noije, P. Le Sager, A. Ito, E. Athanasopoulou, A. Nenes, M. Kanakidou, M. C. Krol, E. Gerasopoulos
Publikováno v:
Geoscientific Model Development, Vol 15, Pp 3079-3120 (2022)
Understanding how multiphase processes affect the iron-containing aerosol cycle is key to predicting ocean biogeochemistry changes and hence the feedback effects on climate. For this work, the EC-Earth Earth system model in its climate–chemistry co
Externí odkaz:
https://doaj.org/article/dafae27496de40a09ae786d54eba29c2
Publikováno v:
Atmospheric Chemistry and Physics, Vol 21, Pp 16869-16891 (2021)
Mineral dust aerosols cool and warm the atmosphere by scattering and absorbing solar (shortwave: SW) and thermal (longwave: LW) radiation. However, significant uncertainties remain in dust radiative effects, largely due to differences in the dust siz
Externí odkaz:
https://doaj.org/article/4198065ebe0f4adaa6b528dd3c8ac88a
Publikováno v:
Atmospheric Chemistry and Physics, Vol 21, Pp 16027-16050 (2021)
The source apportionment of aerosol iron (Fe), including natural and combustion Fe, is an important issue because aerosol Fe can enhance oceanic primary production in the surface ocean. Based on our previous finding that combustion Fe emitted by evap
Externí odkaz:
https://doaj.org/article/eb5f2584225d4dc783bb00fd920634b6