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Decadal trends in Red Sea maximum surface temperature
Ocean warming is a major consequence of climate change, with the surface of the ocean having warmed by 0.11 °C decade(−1) over the last 50 years and is estimated to continue to warm by an additional 0.6 – 2.0 °C before the end of the century(1). However, there is considerable variability in the rate...
| Autores principales: | , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2017
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5557812/ https://www.ncbi.nlm.nih.gov/pubmed/28811521 http://dx.doi.org/10.1038/s41598-017-08146-z |