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: 1,859 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
1,559
225
75
1,859
108
56
59
HTML: 1,559
PDF: 225
XML: 75
Total: 1,859
Supplement: 108
BibTeX: 56
EndNote: 59
Views and downloads (calculated since 28 Jan 2025)
Cumulative views and downloads
(calculated since 28 Jan 2025)
Total article views: 1,503 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
1,208
225
70
1,503
108
56
59
HTML: 1,208
PDF: 225
XML: 70
Total: 1,503
Supplement: 108
BibTeX: 56
EndNote: 59
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: 1,859 (including HTML, PDF, and XML)
Thereof 1,754 with geography defined
and 105 with unknown origin.
Total article views: 1,503 (including HTML, PDF, and XML)
Thereof 1,400 with geography defined
and 103 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...