Table 1 Breakdown of repeated measures surveys (n = 29) used by Davis, et al.3 to project global declines in Gnet when accounting for the season and seasonal bins (H hot, C cold, A all, GBR Great Barrier Reef).
From: Global predictions of coral reef dissolution in the Anthropocene
Location | All | Summer | Autumn | Spring | Winter | Seasonal bin | n |
---|---|---|---|---|---|---|---|
Kaneohe Bay Hawaii | 1 | A | 1 | ||||
2 | H | 2 | |||||
Shiraho Reef, Japan | 3 | 1 | C | 4 | |||
3 | H | 3 | |||||
Palau (reef flat) | 1 | 1 | H | 2 | |||
(lagoon) | 1 | 1 | H | 2 | |||
Lizard Island, GBR | 6 | C | 6 | ||||
1 | H | 1 | |||||
Davies Reef GBR | 2 | C | 2 | ||||
2 | H | 2 | |||||
One Tree Island, GBR | 4 | C | 4 |