| 000 | 01469nam a2200265 4500 | ||
|---|---|---|---|
| 999 |
_c13396 _d13396 |
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| 003 | Pe-LiIGP | ||
| 005 | 20210930165740.0 | ||
| 007 | ta | ||
| 008 | 210930e1970 xxuddddfr|||| 0|0 ||eng d | ||
| 040 |
_apeliigp _bspa _cpeliigp |
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| 041 | _aeng | ||
| 082 | 0 | 4 | _a551.6/K21 |
| 100 | 1 |
_95136 _aKantor, Arthur J. _eautor |
|
| 245 | 1 | 0 | _aObjective estimate of the climatology of very tall convective clouds - a negative report |
| 260 |
_aL.G. Hanscom Field: _bAir Force Cambridge Research Laboratories, _c1970 |
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| 300 |
_a7 páginas: _bgráficas; _c30 cm |
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| 504 | _aIncluye bibliografía | ||
| 520 | _aAn objective method has been developed for determining the occurrence and altitude of tall convective clouds for the purpose of construction of a global climatology of such clouds. The particular computer program selected is the version that produced maximum cloud-top estimates in closest agreement with highest radar precipitation echoes for a three-year period at Miami, Fla., Lake Charles, La., New York, N. Y., and Oklahoma City, Okla. A day-by-day comparison of radar echoes and computed cloud tops reveals such numerous and sufficiently large discrepancies that the computerized parcel method does not appear satisfactory for providing a climatology of convective clouds above 40, 000 ft | ||
| 650 | 1 | 4 |
_95087 _aNUBES |
| 650 | 2 | 4 |
_945 _aCLIMATOLOGÍA |
| 650 | 2 | 4 |
_92148 _aESTRATOSFERA |
| 653 | _aNUBES CONVECTIVAS | ||
| 910 | _aphc | ||
| 942 |
_2ddc _cFO |
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