The evolution of industrial-era warming across the continents and oceans provides a context for future climate change and is important for determining climate sensitivity and the processes that control regional warming. Here we use post-AD 1500 palaeoclimate records to show that sustained industrial-era warming of the tropical oceans first developed during the mid-nineteenth century and was nearly synchronous with Northern Hemisphere continental warming.
Links:
[1] http://admin.indiaenvironmentportal.org.in/feature-article/early-onset-industrial-era-warming-across-oceans-and-continents
[2] http://admin.indiaenvironmentportal.org.in/category/author/nerilie-j-abram
[3] http://admin.indiaenvironmentportal.org.in/category/author/helen-v-mcgregor
[4] http://admin.indiaenvironmentportal.org.in/category/author/jessica-e-tierney-et-al
[5] http://admin.indiaenvironmentportal.org.in/category/journal/nature
[6] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-change
[7] http://admin.indiaenvironmentportal.org.in/category/thesaurus/industry
[8] http://admin.indiaenvironmentportal.org.in/category/thesaurus/global-warming
[9] http://admin.indiaenvironmentportal.org.in/category/thesaurus/oceans-and-seas
[10] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-science
[11] http://admin.indiaenvironmentportal.org.in/category/thesaurus/arctic
[12] http://admin.indiaenvironmentportal.org.in/category/thesaurus/indian-ocean
[13] http://admin.indiaenvironmentportal.org.in/category/thesaurus/north-atlantic-ocean
[14] http://admin.indiaenvironmentportal.org.in/category/thesaurus/green-house-gases