Analyzing Temperature Data from XBT Grid Surveys.

This report considers a set of 78 XBT casts obtained by NAVOCEANO on the second leg of its cruise to the Norwegian Sea, Spring 1981. The data were taken in a grid pattern over a rectangular segment of ocean 66.95 -- 67.40 deg N latitude and -5.60 -- -4.35 deg W longitude, in a day and a half. The su...

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Main Author: Karweit,M
Other Authors: NAVAL OCEAN RESEARCH AND DEVELOPMENT ACTIVITY NSTL STATION MS
Format: Text
Language:English
Published: 1984
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA140685
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA140685
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spelling ftdtic:ADA140685 2023-05-15T17:47:02+02:00 Analyzing Temperature Data from XBT Grid Surveys. Karweit,M NAVAL OCEAN RESEARCH AND DEVELOPMENT ACTIVITY NSTL STATION MS 1984-01 text/html http://www.dtic.mil/docs/citations/ADA140685 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA140685 en eng http://www.dtic.mil/docs/citations/ADA140685 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography *Temperature Norwegian Sea Measurement Bathythermograph data Statistical analysis Isotherms Text 1984 ftdtic 2016-02-19T09:29:19Z This report considers a set of 78 XBT casts obtained by NAVOCEANO on the second leg of its cruise to the Norwegian Sea, Spring 1981. The data were taken in a grid pattern over a rectangular segment of ocean 66.95 -- 67.40 deg N latitude and -5.60 -- -4.35 deg W longitude, in a day and a half. The survey was to measure the spatial properties of the temperature field. This report analyzes the data with that perspective, and focuses on estimating isotherm surfaces as characterizations of the temperature field. The data from each cast are reduced to a set of depths at which the temperatures 0, 1, 2, and 3 dec C occurred. With these depths as data, two techniques are considered for estimating isotherm-depth maps: a two-dimensional Fourier series analysis, and an optimal objective analysis. Calculations of the spatial and temporal correlation of the data indicate that these analyses cannot be legitimately applied; and that a spatial characterization of this area is not possible with this data set. Mean depth and slope statistics for the isotherm depths are given. To complete the work, a discourse on measurement error with XBTs is presented, especially as it relates to the estimation of isotherm depths. Text Norwegian Sea Defense Technical Information Center: DTIC Technical Reports database Norwegian Sea
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Physical and Dynamic Oceanography
*Temperature
Norwegian Sea
Measurement
Bathythermograph data
Statistical analysis
Isotherms
spellingShingle Physical and Dynamic Oceanography
*Temperature
Norwegian Sea
Measurement
Bathythermograph data
Statistical analysis
Isotherms
Karweit,M
Analyzing Temperature Data from XBT Grid Surveys.
topic_facet Physical and Dynamic Oceanography
*Temperature
Norwegian Sea
Measurement
Bathythermograph data
Statistical analysis
Isotherms
description This report considers a set of 78 XBT casts obtained by NAVOCEANO on the second leg of its cruise to the Norwegian Sea, Spring 1981. The data were taken in a grid pattern over a rectangular segment of ocean 66.95 -- 67.40 deg N latitude and -5.60 -- -4.35 deg W longitude, in a day and a half. The survey was to measure the spatial properties of the temperature field. This report analyzes the data with that perspective, and focuses on estimating isotherm surfaces as characterizations of the temperature field. The data from each cast are reduced to a set of depths at which the temperatures 0, 1, 2, and 3 dec C occurred. With these depths as data, two techniques are considered for estimating isotherm-depth maps: a two-dimensional Fourier series analysis, and an optimal objective analysis. Calculations of the spatial and temporal correlation of the data indicate that these analyses cannot be legitimately applied; and that a spatial characterization of this area is not possible with this data set. Mean depth and slope statistics for the isotherm depths are given. To complete the work, a discourse on measurement error with XBTs is presented, especially as it relates to the estimation of isotherm depths.
author2 NAVAL OCEAN RESEARCH AND DEVELOPMENT ACTIVITY NSTL STATION MS
format Text
author Karweit,M
author_facet Karweit,M
author_sort Karweit,M
title Analyzing Temperature Data from XBT Grid Surveys.
title_short Analyzing Temperature Data from XBT Grid Surveys.
title_full Analyzing Temperature Data from XBT Grid Surveys.
title_fullStr Analyzing Temperature Data from XBT Grid Surveys.
title_full_unstemmed Analyzing Temperature Data from XBT Grid Surveys.
title_sort analyzing temperature data from xbt grid surveys.
publishDate 1984
url http://www.dtic.mil/docs/citations/ADA140685
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA140685
geographic Norwegian Sea
geographic_facet Norwegian Sea
genre Norwegian Sea
genre_facet Norwegian Sea
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA140685
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766151264887898112