| 000 | 01052nab a22002657 4500 | ||
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| 001 | H620.91 DEW | ||
| 003 | AR-sfUTN | ||
| 008 | 190909b xx |||p|r|||| 00| 0 spa d | ||
| 040 | _cAR-sfUTN | ||
| 080 | _aH620.91 DEW | ||
| 100 | _aForeman, Ronald John | ||
| 700 | _aEmeis, Stefan | ||
| 700 | _aCañadillas, Beatriz | ||
| 245 | _aThe influence of humidity fluxes on atmospheric stability at fino1: a contrast of two februarys | ||
| 336 |
_2rdacontent _atexto _btxt |
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| 337 |
_2rdamedia _asin mediación _bn |
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| 338 |
_2rdacarrier _avolumen _bnc |
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| 505 | _aAir density gradients are a primary concern for those studying atmospheric turbulence. Lighter air close to the surface is statically unstable, promoting the overturning of the air to correct this imbalance, thus leading to higher levels of turbulence | ||
| 650 | _aHUMIDITY FLUXES | ||
| 650 | _aATMOSPHERIC STABILITY | ||
| 650 | _aFINO1 | ||
| 773 |
_tDewi Magazin _wH620.91 DEW _nS.T.:H620.91 DEW PP4076 _g(nro. 45, Ago. 2014), p. 18-22 |
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| 942 | _cAN | ||
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_c41538 _d41538 |
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