1903.] 



C. Little — Himalayan summer storms. 



243 



and East Bengal, and extended to the south-western districts between 

 the 10th and 11th. Defect was greatest in North Bengal on the 

 11th. Tn South- West Bengal and Orissa there was excess throughout, 

 smallest in the former on the 11th and in the latter on the 12th. The 

 large defect in the Circars on the 13th was probably due to the dis- 

 turbed weather which accompanied the formation of the depression off 

 Orissa and the Circars. 



Table V. 



Giving the pressure change daily from July 1th to July \3th, 1903, arranged 

 to shoiu the iveshvard movement of the disturbance. 





July 

 7th 



July 

 8th 



Jnly 

 9th 



July 

 10th 



July 

 11th 



July 

 12th 



July 

 13th 



Assam 



+ -010" 



-•026" 



-*055" 



+ -068" 



+ -001" 



-•071' 



-•014" 



North Bengal ... 



+ •014 



-•027 



-•082 



+ •062 



+ •015 



-•043 



-•046 



Bihar 



+ •004 



-•014 



-•092 



+ •064 



+ •048 



-•066 



-•016 



United Provinces 



+ •024 



-039 



-•113 



+ •034 



+ •023 



+ •022 



+ ■001 



Punjab 



-•004 



-•050 



-•145 



+ '030 



+ •014 



-•010 



+ •126 



Srinagar 



+ 035 



? 



-•101 



-•019 



+ •008 







+ •004 



Table VI. 



Giving the pressure variation from the normal from July 1th to July \%th 



1903, arranged to show the westward movement of the disturbance. 





July 

 7th 



July 



8th 



July 

 9th 



July 

 10th 



July 

 11th 



July 

 12th 



July 

 13th 



Assam 



+ -014" 



-•011" 



-•080" 



-•014" 



-•014" 



-■076" 



-•100" 



North Bengal ... 



+ •025 



+ •008 



-•078 



-•019 



+ •001 



-•042 



-•084 



Bihar 



+ •005 



-•007 



-•C96 



-•033 



+ •013 



-•052 



-•065 



United Provinces 



+ •013 



-•022 



-'130 



-096 



-•078 



-•062 



-•062 



Punjab 



+ 029 



-•017 



-•118 



-123 



-•112 



-•120 



-027 



Srinagar 



+ •111 



p 



-•039 



-016 



-•013 



+ oso 



+ •104 



Leh 



+ •078 



? 



? 



? 



+ 031 



-•018 



-•023 



The above tables show that the fall of pressure was general aloug 

 the Himalayan range on the 8th and that it continued more rapidly on 



