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: 3,470 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
3,003
348
119
3,470
212
87
85
HTML: 3,003
PDF: 348
XML: 119
Total: 3,470
Supplement: 212
BibTeX: 87
EndNote: 85
Views and downloads (calculated since 28 Jan 2025)
Cumulative views and downloads
(calculated since 28 Jan 2025)
Total article views: 1,904 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
1,448
348
108
1,904
212
87
85
HTML: 1,448
PDF: 348
XML: 108
Total: 1,904
Supplement: 212
BibTeX: 87
EndNote: 85
Views and downloads (calculated since 17 Sep 2025)
Cumulative views and downloads
(calculated since 17 Sep 2025)
Total article views: 1,566 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,555
0
11
1,566
0
0
HTML: 1,555
PDF: 0
XML: 11
Total: 1,566
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: 3,470 (including HTML, PDF, and XML)
Thereof 3,318 with geography defined
and 152 with unknown origin.
Total article views: 1,904 (including HTML, PDF, and XML)
Thereof 1,764 with geography defined
and 140 with unknown origin.
Total article views: 1,566 (including HTML, PDF, and XML)
Thereof 1,554 with geography defined
and 12 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...