Cargando…
Multi-model attribution of upper-ocean temperature changes using an isothermal approach
Both air-sea heat exchanges and changes in ocean advection have contributed to observed upper-ocean warming most evident in the late-twentieth century. However, it is predominantly via changes in air-sea heat fluxes that human-induced climate forcings, such as increasing greenhouse gases, and other...
Autores principales: | Weller, Evan, Min, Seung-Ki, Palmer, Matthew D., Lee, Donghyun, Yim, Bo Young, Yeh, Sang-Wook |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group
2016
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4887871/ https://www.ncbi.nlm.nih.gov/pubmed/27245575 http://dx.doi.org/10.1038/srep26926 |
Ejemplares similares
-
Global ocean synoptic thermocline gradient, isothermal-layer depth, and other upper ocean parameters
por: Chu, Peter C., et al.
Publicado: (2019) -
Long-lasting upper ocean temperature responses induced by intense typhoons in mid-latitude
por: Son, Jun-Hyeok, et al.
Publicado: (2022) -
More-frequent extreme northward shifts of eastern Indian Ocean tropical convergence under greenhouse warming
por: Weller, Evan, et al.
Publicado: (2014) -
The dynamics of the upper ocean /
por: Phillips, Owen M., 1930-
Publicado: (1977) -
Ecological control of nitrite in the upper ocean
por: Zakem, Emily J., et al.
Publicado: (2018)