Full Text Available

Note: Clicking the button above will open the full text document at the original institutional repository in a new window.

Modelling dispersal and connectivity of broadcast spawning corals in the Western Indian Ocean

Coral reef degradation is happening at an alarming rate all over the world due to multiple stressors with elevated sea surface temperature being the root cause. Using the Regional Ocean Modelling System and an individual-based model for the western Indian Ocean, this thesis explored the general circ...

Full description

Saved in:
Bibliographic Details
Main Author: Gamoyo, Majambo J
Other Authors: Reason, Christopher
Format: Thesis
Language:English
Published: Department of Oceanography 2019
Subjects:
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1867613342418337792
access_status_str Open Access
author Gamoyo, Majambo J
author2 Reason, Christopher
author_browse Gamoyo, Majambo J
Reason, Christopher
author_facet Reason, Christopher
Gamoyo, Majambo J
author_sort Gamoyo, Majambo J
collection Thesis
description Coral reef degradation is happening at an alarming rate all over the world due to multiple stressors with elevated sea surface temperature being the root cause. Using the Regional Ocean Modelling System and an individual-based model for the western Indian Ocean, this thesis explored the general circulation patterns (both large and mesoscale) important to dispersal and connectivity of broadcast corals while identifying regions that act as a source of larvae and those that receive larvae. Because habitat destruction and fragmentation through severe bleaching and mortality threaten coral reef health, projected thermal stress from Global Climate Models was explored to quantify future bleaching scenarios that might impact the reproductive timing and larval dispersal. Evaluation of the ROMS configuration for the western Indian Ocean shows that the basin-scale circulation patterns of the region are appropriately captured with the mean volume transports consistent with those derived from observation. Using the eddy detection algorithm, a description of the Southern Gyre as a key aspect of the Somali Current system was identified. The Southern Gyre is associated with barotropic instabilities associated with the northward flowing Somali Current. Rossby waves arriving at the East African coast and the strength of the monsoon winds are also responsible for the evolution and intensification of the gyre. The aggregated trajectories from the Lagrangian model highlight the dominant dispersal pathways and barriers to dispersal following release. The general circulation plays an important role in the dispersal of reef larvae over the study region. At a short pelagic larval duration, most of the released larvae settle back to or near natal reefs, but as the pelagic duration increases, the number of isolated reefs and islands decreases. Even with increased pelagic duration, some reefs (e.g., Agalega and Tromelin) are completely isolated. The mean dispersal distance from release to settlement varied across the region with larvae released along the East African coast dispersed an average of 405 km before settling while those in the Seychelles archipelago dispersed about 101 km. Different blocks of clusters were observed with 16 clusters observed when the pelagic duration is shorter (5 days), compared to seven clusters when the pelagic duration is longer (60 days). The warming trends and bleaching thermal stress shows that among the 636 reef pixels in the study region, about 56% showed positive sea surface temperature trends during the study period (1985- 2016). The frequency of bleaching level thermal stress has also increased over the same period, a tendency that climate models project to continue. Even under optimistic scenarios (such as the Representative Concentration Pathway RCP 4.5), most coral reefs are projected to experience severe bleaching and possible mortality by the 2050s. Low to moderate thermal stress are projected over reefs along the East African coast and near the northwest tip of Madagascar and thus these regions may act as potential climate refugia while increasing the potential of reefs to cope with climate change.
format Thesis
id oai:open.uct.ac.za:11427/29633
institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:34:36.552Z
license_str Not specified — see source repository
provenance_str_mv Harvested via OAI-PMH from UCTD — University of Cape Town Open Access Repository
publishDate 2019
publishDateRange 2019
publishDateSort 2019
publisher Department of Oceanography
publisherStr Department of Oceanography
record_format dspace
source_str UCTD — University of Cape Town Open Access Repository
spelling oai:open.uct.ac.za:11427/29633 Modelling dispersal and connectivity of broadcast spawning corals in the Western Indian Ocean Gamoyo, Majambo J Reason, Christopher Oceanography Coral reef degradation is happening at an alarming rate all over the world due to multiple stressors with elevated sea surface temperature being the root cause. Using the Regional Ocean Modelling System and an individual-based model for the western Indian Ocean, this thesis explored the general circulation patterns (both large and mesoscale) important to dispersal and connectivity of broadcast corals while identifying regions that act as a source of larvae and those that receive larvae. Because habitat destruction and fragmentation through severe bleaching and mortality threaten coral reef health, projected thermal stress from Global Climate Models was explored to quantify future bleaching scenarios that might impact the reproductive timing and larval dispersal. Evaluation of the ROMS configuration for the western Indian Ocean shows that the basin-scale circulation patterns of the region are appropriately captured with the mean volume transports consistent with those derived from observation. Using the eddy detection algorithm, a description of the Southern Gyre as a key aspect of the Somali Current system was identified. The Southern Gyre is associated with barotropic instabilities associated with the northward flowing Somali Current. Rossby waves arriving at the East African coast and the strength of the monsoon winds are also responsible for the evolution and intensification of the gyre. The aggregated trajectories from the Lagrangian model highlight the dominant dispersal pathways and barriers to dispersal following release. The general circulation plays an important role in the dispersal of reef larvae over the study region. At a short pelagic larval duration, most of the released larvae settle back to or near natal reefs, but as the pelagic duration increases, the number of isolated reefs and islands decreases. Even with increased pelagic duration, some reefs (e.g., Agalega and Tromelin) are completely isolated. The mean dispersal distance from release to settlement varied across the region with larvae released along the East African coast dispersed an average of 405 km before settling while those in the Seychelles archipelago dispersed about 101 km. Different blocks of clusters were observed with 16 clusters observed when the pelagic duration is shorter (5 days), compared to seven clusters when the pelagic duration is longer (60 days). The warming trends and bleaching thermal stress shows that among the 636 reef pixels in the study region, about 56% showed positive sea surface temperature trends during the study period (1985- 2016). The frequency of bleaching level thermal stress has also increased over the same period, a tendency that climate models project to continue. Even under optimistic scenarios (such as the Representative Concentration Pathway RCP 4.5), most coral reefs are projected to experience severe bleaching and possible mortality by the 2050s. Low to moderate thermal stress are projected over reefs along the East African coast and near the northwest tip of Madagascar and thus these regions may act as potential climate refugia while increasing the potential of reefs to cope with climate change. 2019-02-18T11:27:06Z 2019-02-18T11:27:06Z 2018 2019-02-13T07:05:04Z Doctoral Thesis Doctoral PhD http://hdl.handle.net/11427/29633 eng application/pdf Department of Oceanography Faculty of Science University of Cape Town
spellingShingle Oceanography
Gamoyo, Majambo J
Modelling dispersal and connectivity of broadcast spawning corals in the Western Indian Ocean
thesis_degree_str Doctoral
title Modelling dispersal and connectivity of broadcast spawning corals in the Western Indian Ocean
title_full Modelling dispersal and connectivity of broadcast spawning corals in the Western Indian Ocean
title_fullStr Modelling dispersal and connectivity of broadcast spawning corals in the Western Indian Ocean
title_full_unstemmed Modelling dispersal and connectivity of broadcast spawning corals in the Western Indian Ocean
title_short Modelling dispersal and connectivity of broadcast spawning corals in the Western Indian Ocean
title_sort modelling dispersal and connectivity of broadcast spawning corals in the western indian ocean
topic Oceanography
url http://hdl.handle.net/11427/29633
work_keys_str_mv AT gamoyomajamboj modellingdispersalandconnectivityofbroadcastspawningcoralsinthewesternindianocean