22 John Eliot — On the occasional Inversian of the Temperature [No. 1, 



The following table (Table IV) gives the differences day by day of 

 the night or minimum temperature at the pairs of stations named in the 

 headings, a negative sign indicating that the night temperature was higher 

 at the hill than at the corresponding plain station. 



Table IV. 



1889. 



Quetta 

 & Jaco- 



Mnrree 



& 

 Eawal 

 Pindi. 



Simla & 

 Ludlii- 



Mussoo- 

 ree & 



Ranikhet 

 & 



Darjee- 



ling & 



Mt. Abn 



& 



Pach- 

 marhi & 

 Eoshan- 



gabad. 





babad. 



ana. 



Roorkee. 



Bareilly. 



Dhubri. 



Deesa. 



Jan. 1 



11-8 



-6-8 



07 



-31 



-4-7 



19-7 



09 



8 



2 



8-8 



-8-4 



-4-1 



-2-6 



-8-7 



17-8 



-30 



4-5 



3 



83 



-12-4 



-2-8 



-5 7 



-10 2 



17-1 



-90 



4-0 



4 



4-8 



-5-4 



-4-6 



-34 



-9-2 



146 



-4'5 



50 



5 



178 



37 



85 



37 



-0-2 



192 



-05 



1-5 



6 



133 



-2-8 



53 



4-1 



23 



196 



-35 



40 



7 



43 



-4-8 



03 



-05 



1-3 



188 



-1-5 



46 



8 



14-3 



-103 



2-0 



-7-0 



-8-7 



168 



09 



-79 



9 



23 



-88 



-1-9 



-7-1 



-62 



178 







5-6 



10 



93 



4-8 



7'5 



47 



-3-2 



192 







61 



11 



133 



07 



68 



179 



93 



190 







36 



12 



16 7 



108 



110 



107 



83 



163 



64 



56 



13 



11-3 



57 



19-4 



23 9 



163 



? 



29 



06 



14 



138 



4-2 



155 



15-7 



14 3 



216 



5-4 



46 



15 



168 



1-9 



93 



9-6 



11-3 



22-3 



5-4 



4 1 



16 



128 



9-2 



' 194 



132 



11-3 



20-7 



59 



51 



17 



20-8 



67 



125 



107 



11-8 



? 



1-5 



26 



18 



25-3 



12 



8-2 



126 



9-3 



168 



35 



11 



19 



15-7 



0-7 



91 



7-6 



9-3 



17-9 



3-4 



36 



20 



213 



-48 



29 



-1-1 



-2-7 



17-8 



4-4 



9-6 



21 



-1-2 



-94 



-7-1 



31 



08 



15-1 



-4-0 



56 



22 



14-2 



15-3 



-2 4 



-55 



-8-2 



168 



-5-0 



46 



23 



143 



11-2 



163 



233 



7-8 



158 



5-4 



-0-4 



24 



143 



6-2 



14 5 



182 



203 



21-3 



10'4 



71 



25 



68 



5-2 



11-5 



14-7 



33 



225 



-0-5 



100 



26 



21-2 



53 



11-3 



123 



63 



173 



-0-5 



26 



27 



206 



78 



89 



74 



43 



180 



1-0 



-1-9 



28 



15-2 



16-8 



11-2 



7-2 



4'3 



198 



49 



56 



29 



16-3 



17-8 



201 



18-4 



168 



17-2 



70 



01 



30 



11-8 



168 



25-2 



21-9 



21-8 



21-2 



11-9 



01 



31 



158 



173 



19 6 



151 



183 



21-7 



13-8 



5-1 



Mean ... 



13-3 



3-1 



82 



7-7 



4-7 



186 



2-0 



3-7 



Normal 



| 136 



2-4 



7-1 



8-5 



6-4 



18-9 



02 



53 



mean 

















Diff. from 

 normal 



j-0-3 



+ 07 



+ 1-1 



-08 



-17 



-0-3 



+ 1-8 



-1-6 



An examination of the preceding data shews that there were three 

 periods in Jannary 1889 during which the minimum temperature of the 

 hill stations was in excess of that at the neighbouring plain stations. 

 These were — 



1st, From the 1st to the 4th. 

 2nd. From the 8th to the 11th. 

 3rd. From the 20th to the 22nd. 

 The abnormal temperature relations were most marked during the 



