Zobrazeno 1 - 10
of 59
pro vyhledávání: '"R. M. Holmes"'
Autor:
A. Francis, R. S. Ganeshram, R. E. Tuerena, R. G. M. Spencer, R. M. Holmes, J. A. Rogers, C. Mahaffey
Publikováno v:
Biogeosciences, Vol 20, Pp 365-382 (2023)
Across the Arctic, vast areas of permafrost are being degraded by climate change, which has the potential to release substantial quantities of nutrients, including nitrogen into large Arctic rivers. These rivers heavily influence the biogeochemistry
Externí odkaz:
https://doaj.org/article/9aa11a65902643de940884b6c582c2dd
Publikováno v:
Geoscientific Model Development, Vol 14, Pp 6445-6466 (2021)
The international Thermodynamic Equation of Seawater 2010 (TEOS-10) defined the enthalpy and entropy of seawater, thus enabling the global ocean heat content to be calculated as the volume integral of the product of in situ density, ρ, and potential
Externí odkaz:
https://doaj.org/article/53b373b9221147cd98cdac67d754aa0e
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 14, Iss 3, Pp n/a-n/a (2022)
Abstract Motivated by recent advances in mapping mesoscale eddy tracer mixing in the ocean we evaluate the sensitivity of a coarse‐resolution global ocean model to a spatially variable neutral diffusion coefficient κn(x, y, z). We gradually introd
Externí odkaz:
https://doaj.org/article/727aec1934e44028afcc6ae674ef4a12
Autor:
A. E. Kiss, A. McC. Hogg, N. Hannah, F. Boeira Dias, G. B. Brassington, M. A. Chamberlain, C. Chapman, P. Dobrohotoff, C. M. Domingues, E. R. Duran, M. H. England, R. Fiedler, S. M. Griffies, A. Heerdegen, P. Heil, R. M. Holmes, A. Klocker, S. J. Marsland, A. K. Morrison, J. Munroe, M. Nikurashin, P. R. Oke, G. S. Pilo, O. Richet, A. Savita, P. Spence, K. D. Stewart, M. L. Ward, F. Wu, X. Zhang
Publikováno v:
Geoscientific Model Development, Vol 13, Pp 401-442 (2020)
We introduce ACCESS-OM2, a new version of the ocean–sea ice model of the Australian Community Climate and Earth System Simulator. ACCESS-OM2 is driven by a prescribed atmosphere (JRA55-do) but has been designed to form the ocean–sea ice component
Externí odkaz:
https://doaj.org/article/a236cf9f85bc4b60a5cea5f14e187154
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 13, Iss 7, Pp n/a-n/a (2021)
Abstract Numerical mixing, defined here as the physically spurious tracer diffusion due to the numerical discretization of advection, is known to contribute to biases in ocean models. However, quantifying numerical mixing is nontrivial, with most stu
Externí odkaz:
https://doaj.org/article/cc773430a2254fe18d986c1b42333af8
Autor:
R. C. Upstill-Goddard, M. E. Salter, P. J. Mann, J. Barnes, J. Poulsen, B. Dinga, G. J. Fiske, R. M. Holmes
Publikováno v:
Biogeosciences, Vol 14, Iss 9, Pp 2267-2281 (2017)
We discuss concentrations of dissolved CH4, N2O, O2, NO3− and NH4+, and emission fluxes of CH4 and N2O for river sites in the western Congo Basin, Republic of Congo (ROC). Savannah, swamp forest and tropical forest samples were collected from the C
Externí odkaz:
https://doaj.org/article/16844066e76d4f7a8ebfd351c1a26f24
Publikováno v:
Biogeosciences, Vol 13, Iss 8, Pp 2279-2290 (2016)
The Kolyma River in northeast Siberia is among the six largest Arctic rivers and drains a region underlain by vast deposits of Holocene-aged peat and Pleistocene-aged loess known as yedoma, most of which is currently stored in ice-rich permafrost thr
Externí odkaz:
https://doaj.org/article/20e41e0d0f37420d9cfe409594785702
Autor:
X. Feng, Ö. Gustafsson, R. M. Holmes, J. E. Vonk, B. E. van Dongen, I. P. Semiletov, O. V. Dudarev, M. B. Yunker, R. W. Macdonald, D. B. Montluçon, T. I. Eglinton
Publikováno v:
Biogeosciences, Vol 12, Iss 15, Pp 4841-4860 (2015)
Hydrolyzable organic carbon (OC) comprises a significant component of sedimentary particulate matter transferred from land into oceans via rivers. Its abundance and nature are however not well studied in Arctic river systems, and yet may represent an
Externí odkaz:
https://doaj.org/article/acff5fc9f0b8428b94e5cd8333372cd0
Publikováno v:
Journal of Climate. 36:2663-2680
Ocean heat uptake is asymmetric with respect to the sign of radiative forcing. It is already known that surface cooling anomalies penetrate into the ocean faster than surface warming anomalies. Because of this asymmetry, the time-variable component o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e13d4fa2b979faeadef1fbd44325a7db
https://doi.org/10.1175/jcli-d-22-0267.1
https://doi.org/10.1175/jcli-d-22-0267.1
Publikováno v:
Journal of Physical Oceanography. 52:981-1014
Microstructure observations in the Pacific cold tongue reveal that turbulence often penetrates into the thermocline, producing hundreds of watts per square meter of downward heat transport during nighttime and early morning. However, virtually all ob
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f146674fac2f39ebdb706bd138bc650b
https://doi.org/10.1175/jpo-d-21-0153.1
https://doi.org/10.1175/jpo-d-21-0153.1