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Medspiration – System Requirements Document - Data User Element

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<strong>Medspiration</strong><br />

MED-SOC-RS-001_1<br />

<strong>System</strong> <strong>Requirements</strong> <strong>Document</strong><br />

Issue F<br />

models. It is never observed directly by satellites, but it comes closest to being<br />

detected by a microwave radiometer which penetrates the skin, at dawn when the<br />

previous day’s diurnal stratification can be assumed to have decayed and<br />

SSTsubskin, SSTdepth and SSTfnd are equal.<br />

Figure 2-1 Schematic diagram showing (a) idealised night-time vertical temperature<br />

deviations from SSTfnd and (b) idealised day-time vertical temperature deviations<br />

from SSTfnd in the upper ocean.<br />

Although the distinctions between the different definitions of SST may seem arcane, they<br />

are very significant when uncertainties of temperature measurement less than 0.3ºC are<br />

being sought.<br />

2.1.2 <strong>Medspiration</strong> SST Products<br />

The <strong>Medspiration</strong> processing system (MPS) will adhere closely to the data processing<br />

model and product specifications defined by the GHRSST-PP [RD.1]. It will produce the<br />

following data products:<br />

• L2P SST products for the European RDAC area which spans from 70S to 90N (to the<br />

ice limit) and from 100W to 45E and contains the whole Atlantic and the adjacent<br />

European seas (see Figure 2-2). Parts of the Pacific Ocean within these limits are<br />

expressly excluded. L2P products consist of the L2 SST data in their native sampling<br />

grid as ingested, with the addition of a quantitative confidence value attached to<br />

every data point. The confidence value will be based on the sensor specific error<br />

© 2004 SOC Page 16 of 193

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