. The climate and weather of Baltimore . O T-i 1-1 to O CO O ?* O CO O M O CO MZ ^ ^^ M t- CO rt CI CO CO OS I—I ^1 1—( 1—I 01 .—( O 1-1 O ^ r/i <u ^ 3 a a D a 3O O ^ X to u u ft 3 a ft O) fl t- ^ ~ _Q) a^ S •- -i-J a a 2S fl 0) 0) tj a§o ^^ T a* ?,, ^ a a a a § . o Cd Ci Cj Pi -M O t- CO t- CO > „> .9 O g a a a; ^ >, t^ o i) S * CS ^ H i a i,333 a a a 3 a r *^ ?3 .5 S I «-) «H oj 0 ?U -M +J %i 3 0 cj 0 0 0 000 3 0) > f> 000 3 Q >> >i >> Q t/) 000 n 3 3 3 0) 0) <D 0) ^ ^ ;-• f4 a ft 0 ft ft ?J !JP CS ew CM ^ 0) 0) -^ ^ 2 S CO 3Q fefafeolPLi Hh (1|Ph[1|« 3 fo
. The climate and weather of Baltimore . O T-i 1-1 to O CO O ?* O CO O M O CO MZ ^ ^^ M t- CO rt CI CO CO OS I—I ^1 1—( 1—I 01 .—( O 1-1 O ^ r/i <u ^ 3 a a D a 3O O ^ X to u u ft 3 a ft O) fl t- ^ ~ _Q) a^ S •- -i-J a a 2S fl 0) 0) tj a§o ^^ T a* ?,, ^ a a a a § . o Cd Ci Cj Pi -M O t- CO t- CO > „> .9 O g a a a; ^ >, t^ o i) S * CS ^ H i a i,333 a a a 3 a r *^ ?3 .5 S I «-) «H oj 0 ?U -M +J %i 3 0 cj 0 0 0 000 3 0) > f> 000 3 Q >> >i >> Q t/) 000 n 3 3 3 0) 0) <D 0) ^ ^ ;-• f4 a ft 0 ft ft ?J !JP CS ew CM ^ 0) 0) -^ ^ 2 S CO 3Q fefafeolPLi Hh (1|Ph[1|« 3 fo ^ 5 S l>^ a £ £00 to 3 3 CI t, 3 3 •- iS ?^^ -a ^ ?3 H p_i >> 3 ^ O H :g S g. M >, g 3 2 P =5 « •- r; O a a C3 « g 3 3 M-l g « a a - § i 1 -s 5 MARYLAND WEATHER SERVICE. VOLUME 2, PLATE CQ 3 X CD oc I- - HJ< . I I- Oz ? I— ± 0- o^o: <Q ? THE WEATHER OF BALTIMORE INTEODUCTION Leaving now the discussion of climate, or the average and extremevalues of the principal factors which constitute the sum total of atmos-pheric conditions, we come to a consideration of some of the more im-portant types of weather characteristic of the geographical horizon ofBaltimore. As stated in the introduction to this report, the term weatheris restricted in its use to the actual state of the atmosphere as regardstemperature, humidity, wind movement, etc., at any given instant, orshort period of time. The method employed in the discussion of cli-matic conditions is not applicable to descriptions of weather; the variousfactors cannot be considered separately, but must be studied in theirrelations to one another at a given instant of time, in order to afford aproper mental picture of actual conditions in nature. The past fifty or sixty years have
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