An evaluation of formulas for estimating clear-sky insolation over the ocean

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049 ⊔ ⊔ ‡aMAIN
050 ⊔ 4 ‡aQC807.5 ‡b.U66 no.352
074 ⊔ ⊔ ‡a208-B-7
086 0 ⊔ ‡aC 55.13:ERL 352-PMEL 26
100 1 ⊔ ‡aReed, Ronald K., ‡eauthor.
245 1 3 ‡aAn evaluation of formulas for estimating clear-sky insolation over the ocean.
264 ⊔ 1 ‡aWashington, DC : ‡bUnited States Government Printing Office, ‡c1975.
300 ⊔ ⊔ ‡a25 pages : ‡billustrations ; ‡c27 cm
336 ⊔ ⊔ ‡atext ‡btxt ‡2rdacontent
337 ⊔ ⊔ ‡aunmediated ‡bn ‡2rdamedia
338 ⊔ ⊔ ‡avolume ‡bnc ‡2rdacarrier
490 0 ⊔ ‡aNOAA technical report ; ‡vERL 352-PMEL 26
500 ⊔ ⊔ ‡a"December 1975."
504 ⊔ ⊔ ‡aIncludes bibliographical references (pages 24-25).
520 3 ⊔ ‡aRecent oceanic data and observations from five coastal sites in the National Weather Service solar radiation network are compared with a formula for computing clear-sky insolation derived from the Smithsonian Meteorological Tables, using a transmission coefficient of 0.7. The results are generally in good agreement, and they suggest that this formula is suitable for computing insolation over the ocean for a wide range of latitudes. The comparison also indicates that a correction to the formula for middle latitudes is not warranted. The one other formula in good agreement with that form the Smithsonian Tables is one derived by Lumb; Laevastu's formula is only acceptable at sun angles less that 50°, and Berliands' estimates are too high at all solar altitudes. The formula from the Smithsonian Tables can be used to compute insolation over the oceans with a random error of estimate probably not exceeding 5% for periods of a few days or longer.
538 ⊔ ⊔ ‡aMode of access: Internet.
650 ⊔ 7 ‡aVisibility. ‡2fast ‡0(OCoLC)fst01167839
650 ⊔ 7 ‡aSolar radiation ‡xStatistical methods. ‡2fast ‡0(OCoLC)fst01125180
650 ⊔ 7 ‡aOcean-atmosphere interaction. ‡2fast ‡0(OCoLC)fst01043612
650 ⊔ 7 ‡aAtmospheric transparency. ‡2fast ‡0(OCoLC)fst00820538
650 ⊔ 6 ‡aInteraction mer-atmosphère.
650 ⊔ 6 ‡aRayonnement solaire ‡xMéthodes statistiques.
650 ⊔ 6 ‡aVisibilité.
650 ⊔ 6 ‡aTransparence de l'air.
650 ⊔ 0 ‡aOcean-atmosphere interaction.
650 ⊔ 0 ‡aSolar radiation ‡xStatistical methods.
650 ⊔ 0 ‡aVisibility.
650 ⊔ 0 ‡aAtmospheric transparency.
700 1 ⊔ ‡aBerli︠a︡nd, M. E., ‡escientist.
700 1 ⊔ ‡aLaevastu, Taivo, ‡escientist.
700 1 ⊔ ‡aLumb, F. E., ‡escientist.
710 1 ⊔ ‡aUnited States. ‡bNational Oceanic and Atmospheric Administration, ‡eissuing agency.
710 2 ⊔ ‡aEnvironmental Research Laboratories (U.S.)
710 2 ⊔ ‡aPacific Marine Environmental Laboratory (U.S.)
CID ⊔ ⊔ ‡a102930647
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