Atlantic Alkenone Sea-Surface Temperature Records

1999 ◽  
pp. 33-55 ◽  
Author(s):  
Ralph R. Schneider ◽  
Peter J. Müller ◽  
Ruth Acheson
Keyword(s):  
Surface Temperature ◽  
Sea Surface Temperature ◽  
Sea Surface ◽  
Temperature Records

scholarly journals Sea-surface temperature records of Termination 1 in the Gulf of California: Challenges for seasonal and interannual analogues of tropical Pacific climate change

2012 ◽  
Vol 27 (2) ◽  
pp. n/a-n/a ◽  
Author(s):  
Erin L. McClymont ◽  
Raja S. Ganeshram ◽  
Laetitia E. Pichevin ◽  
Helen M. Talbot ◽  
Bart E. van Dongen ◽  
...  
Keyword(s):  
Climate Change ◽  
Surface Temperature ◽  
Sea Surface Temperature ◽  
Gulf Of California ◽  
Tropical Pacific ◽  
Sea Surface ◽  
Temperature Records

scholarly journals COASTAL SEA SURFACE TEMPERATURE RECORDS ALONG THE BAJA CALIFORNIA PENINSULA

2012 ◽  
Vol 27 (2) ◽  
pp. 65
Author(s):  
M. T. Sicard -González ◽  
M. A. Tripp -Valdéz ◽  
L. Ocampo ◽  
A. N. Maeda -Martínez ◽  
S. E. Lluch -Cota
Keyword(s):  
Surface Temperature ◽  
Sea Surface Temperature ◽  
Baja California ◽  
Sea Surface ◽  
Baja California Peninsula ◽  
Coastal Sea ◽  
Temperature Records

Registros costeros de temperatura superficial del mar en la Península de Baja California El análisis de series ambientales de temperatura de alta resolución temporal en las zonas costeras permitirá caracterizar mejor las formas y escalas de variación. Las bases de datos disponibles actualmente carecen de suficiente resolución para detectar variaciones ambientales a escalas de horas y días. En este trabajo damos a conocer una colección de registros de alta frecuencia de diversos sitios a lo largo de las costas de la Península de Baja California. Hasta el momento se tienen 47 sitios; sin embargo, esta red de monitoreo pretende expandirse con el objetivo de generar bases de datos de acceso público y gratuito, proporcionando una valiosa herramienta no solo para la investigación, sino también para aplicaciones como la producción acuícola.

Sea surface temperature records in the northern South China Sea from mid-Holocene coral Sr/Ca ratios

2007 ◽  
Vol 22 (3) ◽  
pp. n/a-n/a ◽  
Author(s):  
Gangjian Wei ◽  
Wenfeng Deng ◽  
Kefu Yu ◽  
Xian-hua Li ◽  
Weidong Sun ◽  
...  
Keyword(s):  
South China Sea ◽  
Surface Temperature ◽  
Sea Surface Temperature ◽  
South China ◽  
Northern South China Sea ◽  
Sea Surface ◽  
China Sea ◽  
Temperature Records

High resolution unsaturated alkenones sea surface temperature records in the Yellow Sea during the period of 3500–1300 cal. yr BP

2017 ◽  
Vol 441 ◽  
pp. 107-116 ◽  
Author(s):  
Qingyun Nan ◽  
Tiegang Li ◽  
Jinxia Chen ◽  
Xuefa Shi ◽  
Xinke Yu ◽  
...  
Keyword(s):  
High Resolution ◽  
Surface Temperature ◽  
Sea Surface Temperature ◽  
Yellow Sea ◽  
Sea Surface ◽  
The Yellow Sea ◽  
Temperature Records

scholarly journals Holocene trends in the foraminifer record from the Norwegian Sea and the North Atlantic Ocean

2009 ◽  
Vol 5 (4) ◽  
pp. 2081-2113 ◽  
Author(s):  
C. Andersson ◽  
F. S. R. Pausata ◽  
E. Jansen ◽  
B. Risebrobakken ◽  
R. J. Telford
Keyword(s):  
Surface Temperature ◽  
Sea Surface Temperature ◽  
North Atlantic ◽  
North Atlantic Ocean ◽  
Sea Surface ◽  
Norwegian Sea ◽  
The North ◽  
Temperature Reconstructions ◽  
The North Atlantic ◽  
Temperature Records

Abstract. The early to mid-Holocene thermal optimum is a well-known feature in a wide variety of paleoclimate archives from the Northern Hemisphere. Reconstructed summer temperature anomalies from across northern Europe show a clear maximum around 6 ka. For the marine realm, Holocene trends in sea-surface temperature reconstructions for the North Atlantic and Norwegian Sea do not exhibit a consistent pattern of early to mid-Holocene warmth. Sea-surface temperature records based on alkenones and diatoms generally show the existence of a warm early to mid-Holocene optimum. In contrast, several foraminifer and radiolarian based temperature records from the North Atlantic and Norwegian Sea show a cool mid-Holocene anomaly and a trend towards warmer temperatures in the late Holocene. In this paper, we revisit the foraminifer record from the Vøring Plateau in the Norwegian Sea. We also compare this record with published foraminifer based temperature reconstructions from the North Atlantic and with modelled (CCSM3) upper ocean temperatures. Model results indicate that while the seasonal summer warming of the sea-surface was stronger during the mid-Holocene, sub-surface depths experienced a cooling. This hydrographic setting can explain the discrepancies between the Holocene trends exhibited by phytoplankton and zooplankton based temperature proxy records.

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