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| 001 | 102325943 | ||
| 003 | MiAaHDL | ||
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| 007 | cr bn ---auaua | ||
| 008 | 090421e198006 maua bt f000 0 eng d | ||
| 035 | ⊔ | ⊔ | ‡a(MiU)990161179240106381 |
| 035 | ⊔ | ⊔ | ‡asdr-miu.990161179240106381 |
| 035 | ⊔ | ⊔ | ‡z(MiU)MIU01000000000000016117924-goog |
| 035 | ⊔ | ⊔ | ‡a(OCoLC)318912322 |
| 035 | ⊔ | ⊔ | ‡z(MiU)Aleph016117924 |
| 040 | ⊔ | ⊔ | ‡aLHL ‡beng ‡cLHL ‡dFUG ‡dOCLCQ ‡dTRAAL |
| 049 | ⊔ | ⊔ | ‡aMAIN |
| 086 | 0 | ⊔ | ‡aD 301.45/9:428 |
| 088 | ⊔ | ⊔ | ‡aADA 092447 |
| 088 | ⊔ | ⊔ | ‡aAFGL TR 80-209 |
| 100 | 1 | ⊔ | ‡aBunting, James T. |
| 245 | 1 | 0 | ‡aHorizontal scale variations in satellite estimates of weather erosion parameters for reentry systems / ‡cJames T. Bunting, Chankey N. Touart. |
| 264 | ⊔ | 1 | ‡aHanscom AFB, Massachusetts : ‡bAir Force Geophysics Laboratory, Air Force Systems Command, United States Air Force, ‡c1980. |
| 300 | ⊔ | ⊔ | ‡a27 pages : ‡billustrations, tables ; ‡c28 cm. |
| 336 | ⊔ | ⊔ | ‡atext ‡btxt ‡2rdacontent |
| 337 | ⊔ | ⊔ | ‡aunmediated ‡bn ‡2rdamedia |
| 338 | ⊔ | ⊔ | ‡avolume ‡bnc ‡2rdacarrier |
| 490 | 0 | ⊔ | ‡aAFGL-TR ; ‡v80-0209 |
| 490 | 0 | ⊔ | ‡aAir Force Surveys in Geophysics ; ‡vNo. 428 |
| 500 | ⊔ | ⊔ | ‡aResearch supported by the Air Force Geophysics Laboratory, Air Force Systems Command, United States Air Force, Hanscom AFB, Massachusetts. |
| 500 | ⊔ | ⊔ | ‡aMeteorology Division Project 6670. |
| 500 | ⊔ | ⊔ | ‡aADA092447 (from http://www.dtic.mil). |
| 500 | ⊔ | ⊔ | ‡a"26 June 1980." |
| 504 | ⊔ | ⊔ | ‡aIncludes bibliographical references. |
| 520 | ⊔ | ⊔ | ‡aA weather erosion parameter known as the Environmental Severity Index (ESI) has been estimated using infrared and visible data from satellites. Cloud sampling requirements limited the original prediction equations to satellite data averaged over a horizontal scale of 70 km. Further experiments have demonstrated great utility for satellite estimates on a scale of 10 km and also revealed some systematic differences between the coarse and the fine scale estimates. The ESI averages 1 percent to 10 percent higher for the fine scale estimates and high values of ESI are observed more frequently. (Author). |
| 538 | ⊔ | ⊔ | ‡aMode of access: Internet. |
| 650 | ⊔ | 0 | ‡aAerodynamic heating. |
| 650 | ⊔ | 0 | ‡aPrecipitation (Meteorology) ‡xMeasurement ‡xRemote sensing. |
| 650 | ⊔ | 0 | ‡aInfrared detectors. |
| 650 | ⊔ | 0 | ‡aOptical detectors. |
| 650 | ⊔ | 0 | ‡aMeteorological satellites. |
| 650 | ⊔ | 0 | ‡aClouds ‡xMeasurement ‡xRemote sensing. |
| 650 | ⊔ | 0 | ‡aArtificial satellites ‡xAtmospheric entry. |
| 700 | 1 | ⊔ | ‡aTouart, C. N., ‡eauthor. |
| 710 | 2 | ⊔ | ‡aU.S. Air Force Geophysics Laboratory. |
| 730 | 0 | ⊔ | ‡aTechnical Report Archive & Image Library (TRAIL) |
| 899 | ⊔ | ⊔ | ‡a39015095139690 |
| CID | ⊔ | ⊔ | ‡a102325943 |
| DAT | 0 | ⊔ | ‡b20221206000000.0 |
| DAT | 1 | ⊔ | ‡a20221210060735.0 ‡b2024-04-27T17:32:09Z |
| CAT | ⊔ | ⊔ | ‡aSDR-MIU ‡cmiu ‡dALMA ‡lprepare.pl-004-008 |
| FMT | ⊔ | ⊔ | ‡aBK |
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| 974 | ⊔ | ⊔ | ‡bMIU ‡cGWLA ‡d20240427 ‡sgoogle ‡umdp.39015095139690 ‡y1980 ‡rpd ‡qbib ‡tUS fed doc |