Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 1,483 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
1,333
114
36
1,483
78
40
43
HTML: 1,333
PDF: 114
XML: 36
Total: 1,483
Supplement: 78
BibTeX: 40
EndNote: 43
Views and downloads (calculated since 28 Jan 2025)
Cumulative views and downloads
(calculated since 28 Jan 2025)
Total article views: 1,127 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
982
114
31
1,127
78
40
43
HTML: 982
PDF: 114
XML: 31
Total: 1,127
Supplement: 78
BibTeX: 40
EndNote: 43
Views and downloads (calculated since 17 Sep 2025)
Cumulative views and downloads
(calculated since 17 Sep 2025)
Total article views: 356 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
351
0
5
356
0
0
HTML: 351
PDF: 0
XML: 5
Total: 356
BibTeX: 0
EndNote: 0
Views and downloads (calculated since 28 Jan 2025)
Cumulative views and downloads
(calculated since 28 Jan 2025)
Viewed (geographical distribution)
Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 1,483 (including HTML, PDF, and XML)
Thereof 1,400 with geography defined
and 83 with unknown origin.
Total article views: 1,127 (including HTML, PDF, and XML)
Thereof 1,046 with geography defined
and 81 with unknown origin.
Total article views: 356 (including HTML, PDF, and XML)
Thereof 354 with geography defined
and 2 with unknown origin.
This paper highlights the changes in ocean temperatures and currents that are likely to affect the Great Barrier Reef in coming decades - affecting an iconic and unique environment. It uses newly available high-resolution coupled climate model output to assess the ocean warming and analyses the causes and repercussions of such warming due to climate change.
This paper highlights the changes in ocean temperatures and currents that are likely to affect...
We examined projected changes in Coral Sea temperature and currents through to 2050 using high-resolution CMIP6 models. Surface warming deepened by 30 m per decade, reaching 400 m by 2050. There was sub-surface cooling between 400 and 600 m. North Vanuatu Jet and North Caledonian Jet transports weakened, and the South Caledonian Jet strengthened. These changes may influence western boundary currents and upwelling dynamics on the Great Barrier Reef.
We examined projected changes in Coral Sea temperature and currents through to 2050 using...