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In situ [a] is a Latin phrase meaning "in place" or "on site", derived from in ("in") and situ (ablative of situs, "place"). [3] The term refers to the examination or preservation of phenomena within their original place or context. This methodological approach, used across diverse disciplines, maintains contextual integrity essential for ...
The SeaWiFS Bio-optical Archive and Storage System (SeaBASS) is a data archive of in situ oceanographic data used to support satellite remote sensing research of ocean color. SeaBASS is used for developing algorithms for satellite-derived variables (such as chlorophyll-a concentration ) and for validating or “ground-truthing” satellite ...
In situ observations spanning from the early 1700s to present are available from the International Comprehensive Ocean Atmosphere Data Set (ICOADS). This data set includes observations of a number of the surface ocean and atmospheric variables from ships, moored and drifting buoys and C-MAN stations.
Data useful for operational oceanography, are obtained by diverse means including in-situ (ships, drifters, floats, moorings, etc.) and satellites. They come in very different forms, from a single variable measured at a single point to multivariate, four-dimensional collections of data that can represent data volumes from a few bytes to gigabytes.
Conservative temperature is defined to be directly proportional to potential enthalpy. It is rescaled to have the same units as the in-situ temperature: = where = 3989.24495292815 J kg −1 K −1 is a reference value of the specific heat capacity, chosen to be as close as possible to the spatial average of the heat capacity over the entire ocean surface.
The CORA dataset is designed for operational oceanography, so most global real time monitoring networks are plugged into this database. The data sources are the following: ARGO (autonomous drifting profilers) The global network of moored buoys comprising the TAO/TRITON, [4] PIRATA and RAMA arrays; EGO (underwater gliders)
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The WOA consists of a climatology of fields of in situ ocean properties for the World Ocean. It was first produced in 1994 [ 2 ] (based on the earlier Climatological Atlas of the World Ocean , 1982 [ 3 ] ), with later editions at roughly four year intervals in 1998, 2001, 2005, 2009, 2013, 2018, and 2023.