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by: Eduardo Lowe


Eduardo Lowe
Texas A&M
GPA 3.78

Shaima Nasiri

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About this Document

Shaima Nasiri
Class Notes
25 ?




Popular in Course

Popular in Atmospheric Sciences (ATM S)

This 11 page Class Notes was uploaded by Eduardo Lowe on Wednesday October 21, 2015. The Class Notes belongs to ATMO 201 at Texas A&M University taught by Shaima Nasiri in Fall. Since its upload, it has received 14 views. For similar materials see /class/225940/atmo-201-texas-a-m-university in Atmospheric Sciences (ATM S) at Texas A&M University.

Similar to ATMO 201 at Texas A&M

Popular in Atmospheric Sciences (ATM S)




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Date Created: 10/21/15
water vapor A distribution 30 Sept 2008 1615 UTC Temperature Forecast eatedrSEP 30 1213pm any Dewpoint Forecast aturEF Tue 52p Yue sep so 2005 152 n soscale analysis eatedrSEp so 1213pm Eur WaterVapor P O3 mb T vapor speci c relative TD pressure humidity humidity 24 C75 F 94 mb 2 gkg 649 7 C626 F 9 C 662 F 94 mb 20 gkg 882 7 C 626 F 32 C 896 F 424 mb 272 gkg 892 30 C 856 F 32 C 896 F 94 mb 20 gkg 407 7 C 626 F 4 C 572 F 64 mb 40 gkg 407 09 C 572 F 32 C 896 F 65 mb 40 gkg 37 09 C 572 F online humidity conversions httowwwcactu52000deukunitmasshumshtml Temperature dependence of saturation so 70 r 45 so 7 m 3 a E E E g a 50 r g a 4 a r so 5 B 40 g a g E 5 i a E 30 Q A a a g r 15 g 20 39 10 0 I I l I 40 20 o 20 Temperature quot0 Fig 54 Aguado and Bun Capynghm 2007 Pearson Prennce Hall nc Temperature dependence of saturation Saturahon vapor pressure mb m 0 fix6 Anpmnu omoads uoumnms a 40 20 O 20 Temperature quot0 Fig 54 Aguado and Bun Capynght 2007 Pearson Prermce Hall nc Saturation specific humidity Temperature dependence of saturation Cooling from 30 C to 25 C leads to a change in saturation specific humidity of 73 gkg meaning that much condenses A Specific humidity 73 30 7 7 Specific humidity i 25 7 277 kg g 20 Specmc humidity 204 kg g a 15 Specmc humidity 55 kg AT 5 C Specific C o o 10 g ooling from 5 C to 0 C leads to humldny 3398 k9 A Specific humidity a change in saturation specific 5 17 9 humidity of 17 gkg meaning AT 5 0c kg that much condenses i i i i 30 20 1 D O 10 20 30 40 C 722 e4 14 32 50 68 86 104 F Temperature Capyright 2007 Pearson Prentice Halt inc Box 54 Fig 1 Aguado and Burt UNITED STATES DISTRIBUTION OF FOG 40 i 39 ANNUAL I o I I I I v 4 I w I uq n H mm I I I u I I v I n I I I u I I I I I I I lt I I gt y I I u I I I I I I II I U I 20 w H MEAN DAYS 235 2 WITH 33953 HEAVY FOG In niil 3 TI 2 v 39 OVER 70 39 i 74U7U 30 40 zn3n Iu20 510 1amp5 FIGURE 1Annua1 distribution of the mean number of days with heavy fog from Environmental Data Service NOAA 1971 October 1973 763 W Hardwick I973 MonthlyWeather ReviewVo IO Annual Mean Number of Days with Heavy Fog Visibility S 025 mile I96 I 990 Advection Days Alt55 7 B 55104 0105 154 39 D 155204 ANNUAL I E 205 254 MEAN NUMBER OF DAYS WITH HEAVY FOG 025 MILE Ad d F 255 304 H 355 404 gt 404 from NCDC Climate Maps of the United States Radiation Fog Advection Fog EvaporationMixingSteam Fog zckxon KY Forecast Of ce UPSIOPe Fog


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