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http://nopr.niscpr.res.in/handle/123456789/38794Full metadata record
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Rao, G R Lakshmana | - |
| dc.contributor.author | Prasad, M V Ravi | - |
| dc.date.accessioned | 2016-12-16T09:53:33Z | - |
| dc.date.available | 2016-12-16T09:53:33Z | - |
| dc.date.issued | 1984-09 | - |
| dc.identifier.issn | 0975-1033 (Online); 0379-5136 (Print) | - |
| dc.identifier.uri | http://nopr.niscair.res.in/handle/123456789/38794 | - |
| dc.description | 131-133 | en_US |
| dc.description.abstract | Attempt has been made to obtain sea surface temperature (SST) from routine observations of dry bulb and dew point temperatures and pressure of air at 10 m height above the sea surface using Bowen's ratio, viz. β = 0.63 + 0.63 – 0.15 has been used to obtain SST where γ is the ratio of specific heat of air at constant pressure and latent heat of evaporation at SST and F is the slope of the saturated specific humidity curve at SST. The present method is more suitable for calculating SST. | en_US |
| dc.language.iso | en_US | en_US |
| dc.publisher | NISCAIR-CSIR, India | en_US |
| dc.rights | CC Attribution-Noncommercial-No Derivative Works 2.5 India | en_US |
| dc.source | IJMS Vol.13(3) [September 1984] | en_US |
| dc.title | Calculation of sea surface temperature using meteorological parameters | en_US |
| dc.type | Article | en_US |
| Appears in Collections: | IJMS Vol.13(3) [September 1984] | |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| IJMS 13(3) 131-133.pdf | 508.99 kB | Adobe PDF | View/Open |
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+ 0.63
– 0.15 has been used to obtain SST where γ is the ratio of specific heat of air at constant pressure and latent heat of evaporation at SST and F is the slope of the saturated specific humidity curve at SST. The present method is more suitable for calculating SST.