dc.contributor.author | Seip, Knut Lehre | en_US |
dc.date.accessioned | 2015-04-29T08:10:33Z | |
dc.date.available | 2015-04-29T08:10:33Z | |
dc.date.issued | 2015-03-19 | en_US |
dc.identifier.citation | Seip, K. (2014). Temperature, growth season length and phytoplankton abundance in the Gulf of Maine. Marine and Freshwater Research. | en_US |
dc.identifier.issn | 1323-1650 | en_US |
dc.identifier.other | FRIDAID 1169437 | en_US |
dc.identifier.uri | https://hdl.handle.net/10642/2581 | |
dc.description.abstract | I show that the relation between annual average phytoplankton concentration (as mg Chl-a.m-3) and in situ sea surface temperature, SST, is positive (Chl-a â 0.5 Ã SST, r = 0.8, p < 0.001) at an average temperature of 11oC (range 10oC â 12oC) in the Gulf of Maine. However, within seasonal observations 2005-2009 were predominant negatively associated. For the first, annual average relationship, the extension of the growth season with increasing temperature may be an important factor. I show that an increase by 1oC start the growth season 8 days earlier and lengthen the season with 13 days (temp > 10oC). Tentative calculations suggest that the increased length matches the increase in annual phytoplankton concentration. For the second, negative relationship, I suggest that warmer water during late summer increases stratification and limits nutrient supply to the upper productive layer. | en_US |
dc.language.iso | eng | en_US |
dc.publisher | CSIRO Publishing | en_US |
dc.relation.ispartofseries | Marine & Freshwater Research; | en_US |
dc.subject | Phytoplankton | en_US |
dc.subject | Chl - a | en_US |
dc.subject | Temperature | en_US |
dc.subject | Growth season | en_US |
dc.subject | Coastal region | en_US |
dc.subject | Gulf of Maine | en_US |
dc.title | Temperature, growth season length and phytoplankton abundance in the Gulf of Maine | en_US |
dc.type | Journal article | en_US |
dc.type | Peer reviewed | en_US |
dc.description.version | Postprint version of published article. | en_US |
dc.identifier.doi | http://dx.doi.org/10.1071/MF14034 | |