| LDR | 02567cam a2200445Ii 4500 | ||
| 001 | 102325868 | ||
| 003 | MiAaHDL | ||
| 005 | 20221206000000.0 | ||
| 006 | m d | ||
| 007 | cr bn ---auaua | ||
| 008 | 090421e197903 maua bt f000 0 eng d | ||
| 035 | ⊔ | ⊔ | ‡a(MiU)990161178480106381 |
| 035 | ⊔ | ⊔ | ‡asdr-miu.990161178480106381 |
| 035 | ⊔ | ⊔ | ‡z(MiU)MIU01000000000000016117848-goog |
| 035 | ⊔ | ⊔ | ‡a(OCoLC)318904200 |
| 035 | ⊔ | ⊔ | ‡z(MiU)Aleph016117848 |
| 037 | ⊔ | ⊔ | ‡b22161 |
| 040 | ⊔ | ⊔ | ‡aLHL ‡beng ‡cLHL ‡dFUG ‡dOCLCQ ‡dTRAAL |
| 049 | ⊔ | ⊔ | ‡aMAIN |
| 086 | 0 | ⊔ | ‡aD 301.45/9:408 |
| 088 | ⊔ | ⊔ | ‡aADA 077022 |
| 088 | ⊔ | ⊔ | ‡aAFGL TR 79-79 |
| 100 | 1 | ⊔ | ‡aTattelman, Paul. |
| 245 | 1 | 0 | ‡aClimatic chamber tests of a surface ice accretion measurement system / ‡cPaul Tattelman. |
| 264 | ⊔ | 1 | ‡aHanscom AFB, Massachusetts : ‡bAir Force Geophysics Laboratory, Air Force Systems Command, United States Air Force, ‡c1979. |
| 300 | ⊔ | ⊔ | ‡a50 pages : ‡billustrations ; ‡c28 cm. |
| 336 | ⊔ | ⊔ | ‡atext ‡btxt ‡2rdacontent |
| 337 | ⊔ | ⊔ | ‡aunmediated ‡bn ‡2rdamedia |
| 338 | ⊔ | ⊔ | ‡avolume ‡bnc ‡2rdacarrier |
| 490 | 0 | ⊔ | ‡aAFGL-TR ; ‡v79-0079 |
| 490 | 0 | ⊔ | ‡aAir Force Surveys in Geophysics ; ‡vNo. 408 |
| 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 | ⊔ | ⊔ | ‡aADA077022 (from http://www.dtic.mil). |
| 500 | ⊔ | ⊔ | ‡a"26 March 1979." |
| 504 | ⊔ | ⊔ | ‡aIncludes bibliographical references (pages 49-50). |
| 520 | ⊔ | ⊔ | ‡aClimatic chamber tests of an off-the-shelf ice detection system manufactured by Rosemount Engineering Company were conducted to evaluate its capability to determine ice amounts measured on cylinders. One-hour tests were run for a variety of windspeeds, temperatures, and icing conditions. Some longer duration tests, up to 17 hours, were also performed. Analysis of the data indicates that the Rosemount system is highly correlated with the mass of ice measured on the cylinders when the data are divided into freezing rain and rime icing events. The Rosemount system is also highly correlated with ice thickness, but without the pronounced dependence upon the type of icing. In the light of positive test results, a method is proposed for utilizing the Rosemount system for observing ice accretion at the earth's surface. (Author). |
| 538 | ⊔ | ⊔ | ‡aMode of access: Internet. |
| 650 | ⊔ | 0 | ‡aDetectors. |
| 650 | ⊔ | 0 | ‡aMeteorological instruments. |
| 650 | ⊔ | 0 | ‡aIcing (Meteorology) ‡xSurfaces. |
| 650 | ⊔ | 0 | ‡aIcing (Meteorology) ‡xMeasurement. |
| 710 | 2 | ⊔ | ‡aU.S. Air Force Geophysics Laboratory. |
| 730 | 0 | ⊔ | ‡aTechnical Report Archive & Image Library (TRAIL) |
| 899 | ⊔ | ⊔ | ‡a39015095138940 |
| CID | ⊔ | ⊔ | ‡a102325868 |
| DAT | 0 | ⊔ | ‡b20221206000000.0 |
| DAT | 1 | ⊔ | ‡a20221210060735.0 ‡b2024-04-28T17:30:14Z |
| CAT | ⊔ | ⊔ | ‡aSDR-MIU ‡cmiu ‡dALMA ‡lprepare.pl-004-008 |
| FMT | ⊔ | ⊔ | ‡aBK |
| HOL | ⊔ | ⊔ | ‡0sdr-miu.990161178480106381 ‡aMiU ‡bSDR ‡cGWLA ‡f016117848 ‡pmdp.39015095138940 ‡sMIU ‡1990161178480106381 |
| 974 | ⊔ | ⊔ | ‡bMIU ‡cGWLA ‡d20240428 ‡sgoogle ‡umdp.39015095138940 ‡y1979 ‡rpd ‡qbib ‡tUS fed doc |