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Tellus A Dynamic Meteorology and Oceanography is a peer-reviewed journal published by Wiley, covering Meteorological Phenomena and Simulations, Climate variability and models, Oceanographic and Atmospheric Processes.
| Publisher | Wiley |
|---|---|
| Reference style | Author–year (Chicago) Author–year — (Smith, 2023) in the text Smith, Ada, Ben Jones, and Cara Lee. 2023. "A Representative Article Title." Tellus A Dynamic Meteorology and Oceanography 12 (3): 45–58.
Formats any DOI in Tellus A Dynamic Meteorology and Oceanography style. No sign-up. |
| Publishes research in | Meteorological Phenomena and Simulations Climate variability and models Oceanographic and Atmospheric Processes Tropical and Extratropical Cyclones Research Geophysics and Gravity Measurements |
| ISSN | 0280-6495 |
| Citation impact (2-yr) | 1.94 |
| h-index | 159 |
| i10-index | 2,866 |
| Total citations | 172,914 |
| Article processing charge | $1,410 |
| Open access | Yes |
| Top institutions publishing here | National Institute of Meteorology |
| Journal website | www.tellusa.net |
| You get | A submission-ready PDF and the editable LaTeX source — ready to submit. |
Citations each year’s papers have accumulated so far — the most recent years are still building up.
In chapter 2 the isotopic fractionation of water in some simple condensation-evaporation processes are considered quantitatively on the basis of the fractionation factors given in section 1|2. The condensation temperature is an important parameter, which has got some glaciological applications. The temperature effect (the δ's decreasing with temperature) together with varying evaporation and exchange appear…
A stochastic model of climate variability is considered in which slow changes of climate are explained as the integral response to continuous random excitation by short period “weather” isturbances. The coupled ocean-atmosphere-cryosphere-land system is divided into a rapidly varying “weather” system (essentially the atmosphere) and a slowly responding “climate” system (the ocean, cryosphere, land vegetation,…
Two general algorithms for solving constrained minimization problems are presented and discussed in the context of analysis and assimilation of meteorological observations. In both algorithms, the original constrained problem is transformed by appropriate modifications into one unconstrained problem, or into a sequence of unconstrained problems. The main advantage of proceeding in this way is that…
Free convection between two interconnected reservoirs, due to density differences maintained by heat and salt transfer to the reservoirs, is shown to occur sometimes in two different stable regimes, and may possibly be analogous to certain features of the oseanic circulation.
The available potential energy of the atmosphere may be defined as the difference between the total potential energy and the minimum total potential energy which could result from any adiabatic redistribution of mass. It vanishes if the density stratification is horizontal and statically stable everywhere, and is positive otherwise. It is measured approximately by a…
