1b:I[42426,["/_next/static/immutable/chunks/1xctgzqre-wsy.js","/_next/static/immutable/chunks/06_-wz6pdtp2b.js","/_next/static/immutable/chunks/30e52g49hg40p.js","/_next/static/immutable/chunks/02yq6tul2z-oh.js","/_next/static/immutable/chunks/10bx_ec2vj7n_.js","/_next/static/immutable/chunks/33bfn03fo8xnt.js","/_next/static/immutable/chunks/0tfjf78scu61b.js","/_next/static/immutable/chunks/31xnvej4n1bi9.js"],"default"] 1c:T45b,

Data were downloaded in the lab and converted to tab delimited text files. Data were quality controlled and trimmed to fit accurate temperature recordings and cut to minimize the data gaps between collection and deployment of new loggers. After deployment the loggers took approximately 2 hours to equilibrate to ambient water temperature. Comparison between the temperature data on a logger just prior to collection and the temperature data at the time of deployment for a logger collected the following month were used to identify accurate data measurements and outliers were removed from the data set. Occasionally an entire record for a particular depth was lost due to instrument failure.

Files were named labeled with a letter indicating which depth in the water column they were collected (S=surface (0.5 m), T=top (4.8 m), M=Middle (8 m), B=bottom (13.5 m)). Dates in the file names indicate the dates of deployment to retrieving the tidbits.

Missing Dates:
Surface - June 2010 to September 2010
Top - July 2012 to September 2012
Mid - September 2011 to December 2011

1d:Taa9,NSF Award Abstract: Kelps inhabit a narrow band of the Earth's ocean margins, yet they sustain some of the most diverse and productive ecosystems on the planet. Despite over 50 years of intensive field and laboratory research, however, much remains to be understood about the processes that determine the dynamics of kelp populations, and the subsequent consequences for the diversity and productivity of their associated communities. This limitation is due largely to the fact that processes regulating kelp system productivity, dynamics, and diversity are determined by how different kelp species interact with environmental variability over ecological and evolutionary timescales. In the face of imminent ocean climate change, how will individual kelp taxa respond to rising ocean temperatures or decreasing nutrients? This project will use a combination of laboratory and field studies to understand interactive effects of changing temperature and nutrients on gametogenesis, fertilization, and sporophyte recruitment of kelp. This project will use 9 kelp taxa from California, British Columbia, Australia, Mexico, South Africa, and Chile to test for local adaptation vs. phylogenetic patterns in these traits and to understand whether the level of stress experienced by a population determines regional tolerance patterns. The project will integrate research activities into a novel curriculum at Moss Landing Marine Laboratory and will involve students in laboratory and field studies. These activities will help students to develop good laboratory skills and facilitate the development of critical-thinking as it pertains to the comparative analysis of kelp life histories, conceptual models of life history evolution, and ecological implications of climate change. Publications resulting from this research: Demes, K.W., Graham, M.H., and Suskiewicz, T.S. 2009. Phenotypic plasticity reconciles incongruous molecular and morphological taxonomies: The giant kelp, Macrocystis (Laminariales, Phaeophyceae), is a monospecific genus. Journal of Phycology, v.45, p. 1266. doi: 10.1111/j.1529-8817.2009.00752.x Demes, K. W. and Graham, M. H. 2011. Abiotic regulation of investment in sexual verus vegetative reproduction in the clonal kelp Laminaria sinclairii (Laminariales, Phaeophyceae). Journal of Phycology, v.47. doi: 10.1111/j.1529-8817.2011.00981.x Henriquez, L.A., Buschmann, A.H., Maldonado, M.A., Graham, M.H., Hernandez-Gonzalez, M.C., Pereda, S.V., and Bobadilla, M.I. 2011. Grazing on giant kelp microscopic phases and the recruitment success of annual populations of Macrocystis pyrifera (Laminariales, Phaeophyceae) in southern Chile. Journal of Phycology, v.47, p. 252. doi: 10.1111/j.1529-8817.2010.00955.x6:["$","$L1b",null,{"dataset":{"_id":"4049","description":"

Temperature data from 4 depths at the study site in the giant kelp forest habitat of the Central California Coast. Temperature was recorded every 5 minutes from June 2010 to October 2012.

\n","problem":"","acquisition":"

Onset Stowaway Tidbits (+/- 0.2C) were positioned at 0.5, 4.8, 8, and 13.5 m along a mooring line at the study site. The loggers were set to record temperature every 5 minutes and were swapped out approximately every 3 months by divers.

Related publications and references:
\nFox, M.D. 2013 Resource translocation drives d13C fractionation during recovery from disturbance in giant kelp, Macrocystis pyrifera. Journal of Phycology 49(5), 811-815. DOI: 10.1111/jpy.12099

\n","processing":"$1c","bcodmoProcessing":"","title":"Temperature time-series data from 4 depths in the Central California kelp forest, measured at the Stillwater Cove Mooring from 2010-2012 (Climate Change Kelp project)","nickname":"Stillwater Cove temperature time series","dataUrl":"","currentState":"Final no updates expected","currentStateId":"7","validated":true,"restricted":false,"version":"1","version_date":"2014-01-24T05:00:00.000Z","abstract":"Temperature data from 4 depths at the study site in the giant kelp forest habitat of the Central California Coast. Temperature was recorded every 5 minutes from June 2010 to October 2012.","citation":"Graham, M., Harley, C. (2014) Temperature time-series data from 4 depths in the Central California kelp forest, measured at the Stillwater Cove Mooring from 2010-2012 (Climate Change Kelp project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2014-01-24 [if applicable, indicate subset used]. doi:10.1575/1912/bco-dmo.4049.1 [access date]","citationParts":{"identifier":"doi:10.1575/1912/bco-dmo.4049.1","versionDate":"2014-01-24","versionId":"1","year":"2014","title":"Temperature time-series data from 4 depths in the Central California kelp forest, measured at the Stillwater Cove Mooring from 2010-2012 (Climate Change Kelp project)","authors":"Graham, M., Harley, C.","publisher":"Biological and Chemical Oceanography Data Management Office (BCO-DMO)."},"doi":"10.1575/1912/bco-dmo.4049.1","release_date":null,"field_dataset_location":"","temporal_extent":{"start":"2010-06-14T04:00:00.000Z","end":"2012-09-28T04:00:00.000Z"},"temporal":{"resolution":"time:unitDay","type":"time:Interval","start":{"value":"1276488000","label":"2010-06-14"},"end":{"value":"1348804800","label":"2012-09-28"}},"spatial_extent":{"shape":"point","center":{"latitude":36.560731,"longitude":-121.9459},"wkt":" POINT (-121.9459 36.560731)","north":0,"east":0,"south":0,"west":0},"dataset_type":["Other Field Results"],"keywords":["oceans"],"data_files":[{"id":"899967","title":"stillwater_cove_temp.csv","url":"https://datadocs.bco-dmo.org/dataset/4049/file/5AAMvOEfz2Wko/stillwater_cove_temp.csv","showTableUrl":"https://www.bco-dmo.org/dataset/4049/data/view/899967","description":"Primary data file for dataset ID 4049","filename":"stillwater_cove_temp.csv","bytesize":126793142,"checksum":{"value":"edbfcd83750b8ebfc0bef2bd29d50aaf","Algorithm":{"_id":"190","name":"MD5"}},"mimetype":"text/csv","fileType":{"_id":"192","name":"Comma Separated Values (.csv)"},"isErddap":"bcodmo_dataset_4049","date":"","isPublicDuringEmbargo":false,"primaryDataFile":true,"showTable":true,"restricted":false}],"supplemental_files":[],"roles":[{"role":{"_id":"138","name":"Principal Investigator"},"performedBy":{"_id":"51718","name":"Michael H Graham"},"performedAtOrganization":{"_id":"79","name":"Moss Landing Marine Laboratories"}},{"role":{"_id":"140","name":"Co-Principal Investigator"},"performedBy":{"_id":"51727","name":"Professor Christopher Harley"},"performedAtOrganization":{"_id":"344","name":"University of British Columbia"}},{"role":{"_id":"133","name":"Contact"},"performedBy":{"_id":"51728","name":"Arley Muth"},"performedAtOrganization":{"_id":"79","name":"Moss Landing Marine Laboratories"}},{"role":{"_id":"145","name":"BCO-DMO Data Manager"},"performedBy":{"_id":"51498","name":"Shannon Rauch"},"performedAtOrganization":{"_id":"191","name":"Woods Hole Oceanographic Institution"}}],"deployments":[{"_id":"59094","name":"SCove_Moor_MHG","synonyms":[],"dates":{"start":"2010-06-14T00:00:00.000Z","end":"2012-10-03T00:00:00.000Z"},"platform":{"_id":"54282","name":"Stillwater Cove Mooring"},"chiefScientists":[]}],"funding":[{"_id":"55205","name":"OCE-0752523","fundingSource":{"_id":"355","name":"NSF Division of Ocean Sciences"},"url":"https://www.nsf.gov/awardsearch/show-award?AWD_ID=0752523"}],"instruments":[{"_id":"6318","name":"Water Temperature Sensor","description":"Onset Stowaway Tidbits (+/- 0.2C) were deployed at 0.5, 4.8, 8, and 13.5 meters depth.","type_id":"647","type_name":"Water Temperature Sensor","type_desc":"General term for an instrument that measures the temperature of the water with which it is in contact (thermometer).","type_acronym":"Water Temp Sensor"}],"parameters":[{"_id":"36567","name":"site","format":"","frictionlessType":"","description":"

Name of the study site.

","units":{"_id":"","name":"text"},"type":{"_id":"1124","name":"site","description":"

Sampling site identification.

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Description of the study site.

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Description or characteristics of a sampling site

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Latitude of the study site.

","units":{"_id":"","name":"decimal degrees"},"type":{"_id":"730","name":"latitude","description":"

latitude, in decimal degrees, North is positive, negative denotes South; Reported in some datasets as degrees, minutes

"}},{"_id":"36570","name":"lon","format":"","frictionlessType":"","description":"

Longitude of the study site.

","units":{"_id":"","name":"decimal degrees"},"type":{"_id":"731","name":"longitude","description":"

longitude, in decimal degrees, East is positive, negative denotes West; Reported in some datsets as degrees, minutes

"}},{"_id":"36571","name":"depth","format":"","frictionlessType":"","description":"

Depth in the water column at which the temperature logger was positioned.

","units":{"_id":"","name":"meters"},"type":{"_id":"808","name":"depth","description":"

Observation/sample depth below the sea surface. Units often reported as: meters, feet.

\nWhen used in a JGOFS/GLOBEC dataset the depth is a best estimate; usually but not always calculated from pressure; calculated either from CTD pressure using Fofonoff and Millard (1982; UNESCO Tech Paper #44) algorithm adjusted for 1980 equation of state for seawater (EOS80) or simply equivalent to nominal depth as recorded during sampling if CTD pressure was unavailable.

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Description of the depth within the water column at which the temperature logger was positioned.

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description of water mass where sample was collected, for example, mixed layer or deep chlorophyll maximum.

"}},{"_id":"36573","name":"month_local","format":"","frictionlessType":"","description":"

2-digit month (Pacific Standard Time) of the temperature record in mm (01 to 12) format.

","units":{"_id":"","name":"unitless"},"type":{"_id":"895","name":"month_local","description":"

month of year, local time

"}},{"_id":"36574","name":"year_local","format":"","frictionlessType":"","description":"

4-digit year (Pacific Standard Time) of the temperature record in YYYY format.

","units":{"_id":"","name":"unitless"},"type":{"_id":"1062","name":"year","description":"

year, reported as YYYY, e.g. 1995

"}},{"_id":"36575","name":"day_local","format":"","frictionlessType":"","description":"

2-digit day (Pacific Standard Time) of the temperature record in dd (01 to 31) format.

","units":{"_id":"","name":"unitless"},"type":{"_id":"803","name":"day_local","description":"

day, local time

"}},{"_id":"36576","name":"time_local","format":"","frictionlessType":"","description":"

Local time (Pacific Standard Time) in hours, minutes, and decimal minutes of the temperature record in HHMM.mm format.

","units":{"_id":"","name":"unitless"},"type":{"_id":"1007","name":"time_local","description":"

time of day, local time, using 2400 clock format

"}},{"_id":"36577","name":"temp","format":"","frictionlessType":"","description":"

Water temperature in degrees Celsius.

","units":{"_id":"","name":"degrees Celsius"},"type":{"_id":"733","name":"temperature","description":"

water temperature at measurement depth

"}},{"_id":"36578","name":"ISO_DateTime_Local","format":"","frictionlessType":"","description":"

Date and time formatted to ISO8601 standard. Dates and times are local (Pacific Standard Time) in YYYY-mm-ddTHH:MM:SS.ss format.

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Date/Time (Local) ISO formatted
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\nYYYY-MM-DDTHH:MM:SS[.xx]
\n2009-08-30T09:05:00[.xx] (local time)
\n2009-08-30T14:05:00[.xx]Z (UTC time)
\n2009-08-30T14:05:00[.xx]-05:00
\nThe dashes and the colons can be dropped.
\nThe T can also be dropped \"by mutual agreement\", but one needs the trailing Z if the time is UTC.

Note the Time Zone (TZ) as +/-HH:MM
\nTime Zone signage is for conversion from local to UTC
\nWest Coast USA in summer is +7 (add 7 hrs to local time for UTC)

"}},{"_id":"471707","name":"yrday_local","format":"","frictionlessType":"","description":"

Local day and decimal time, as 326.5 for the 326th day of the year at noon, or November 22 at 1200 hours.

","units":{"_id":"","name":"dimensionless"},"type":{"_id":"1069","name":"yrday_local","description":"

local day and decimal time, as 326.5 for the 326th day of the year, or November 22 at 1200 hours (noon)

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