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COADS Release 2 data and metadata enhancements for improvements of marine surface flux fields

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TLDR
The Comprehensive Ocean-Atmosphere Data Set (COADS) as discussed by the authors has been updated through a cooperative U.S. project since 1981, including vital international contributions, and it covers 142 years, 1854-1995.
Abstract
The Comprehensive Ocean-Atmosphere Data Set (COADS) has been updated through a cooperative U.S. project since 1981, including vital international contributions. Quality controlled marine surface observations from ships have been supplemented in more recent years to include moored environmental buoys, drifting buoys, and near-surface measurements from oceanographic profiles. The data set now covers 142 years, 1854–1995. Monthly statistics of pseudo-fluxes and basic marine variables are calculated for each year using observed data falling within 2° latitude × 2° longitude boxes (1°×1° summaries are also available for 1960-93). Enhancements in data and metadata planned by the year 2000 as part of COADS Release 2 (∼ 1820–1997) will concentrate on the basic observational records. In addition to new data sources, which will augment flux estimates through expanded coverage, planned enhancements include: a) usage of selected metadata from WMO Pub. No. 47 (ship instrumentation history) to improve the observational records back to about 1973; b) improvements in the reliability of the wind speed (“estimated/measured”) indicator; and c) bias adjustments of wind speed Beaufort estimates and anemometer measurements.

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Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century

TL;DR: HadISST1 as mentioned in this paper replaces the global sea ice and sea surface temperature (GISST) data sets and is a unique combination of monthly globally complete fields of SST and sea ice concentration on a 1° latitude-longitude grid from 1871.
Journal ArticleDOI

An Improved In Situ and Satellite SST Analysis for Climate

TL;DR: A weekly 1° spatial resolution optimum interpolation (OI) sea surface temperature (SST) analysis has been produced at the National Oceanic and Atmospheric Administration (NOAA) using both in situ and satellite data from November 1981 to the present as mentioned in this paper.
Journal ArticleDOI

The JRA-25 Reanalysis

TL;DR: A long-term global atmospheric reanalysis, named "Japanese 25-year Reanalysis (JRA-25) was completed using the Japan Meteorological Agency (JMA) numerical assimilation and forecast system.
Journal ArticleDOI

Improved Extended Reconstruction of SST (1854–1997)

TL;DR: In this paper, an improved SST reconstruction for the 1854-1997 period is developed, which uses sea ice concentrations to improve the high-latitude SST analysis and a modified historical bias correction for the 1939-41 period.
References
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The NCEP/NCAR 40-Year Reanalysis Project

TL;DR: The NCEP/NCAR 40-yr reanalysis uses a frozen state-of-the-art global data assimilation system and a database as complete as possible, except that the horizontal resolution is T62 (about 210 km) as discussed by the authors.
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Improved Global Sea Surface Temperature Analyses Using Optimum Interpolation

TL;DR: The new NOAA operational global sea surface temperature (SST) analysis is described in this paper, which uses 7 days of in situ (ship and buoy) and satellite SST.
Journal ArticleDOI

A Comprehensive Ocean-Atmosphere Data Set

TL;DR: The Comprehensive Ocean-Atmosphere Data Set (COADS) as mentioned in this paper is the result of a cooperative project to collect global weather observations taken near the ocean surface since 1854, primarily from merchant ships, into a compact and easily used data set.
Journal ArticleDOI

Reconstruction of Historical Sea Surface Temperatures Using Empirical Orthogonal Functions

TL;DR: In this article, a principal component analysis (PCA) was used to improve the accuracy of the NCDC's optimum interpolation (OI) analysis of sea surface temperature (SST) from 1950 to 1981.

World Ocean Atlas 1994. Volume 4. Temperature

TL;DR: In this article, the authors presented maps of in situ temperature at selected levels of the world ocean on a one-degree grid, and presented all-data annual and seasonal compositing periods are presented.
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