172 C. Little — The Himalayan summer storm of iSept. 24thj 1903. [No. 4, 



These tables show a general fall of pressure along the Himalayan 

 range on the 23rd and 24th. The only indication of any westward 

 movement is the recovery of pressure on the 25th in Assam, North 

 Bengal and Bihar, and on the 26th in the United Provinces and the 

 Punjab. 



One matter which may deserve special comment is the rather large 

 defect on the 27th in the Punjab and at Srinagar. It has been pointed 

 out in a previous paper that there appears to be the same tendency to 

 the formation of a cyclonic arrangement of winds in the Punjab after 

 one of these disturbances as in Lower Bengal and the north of the Bay. 

 The deficiency noticed above may be the indication of that tendency in 

 the present case. If so, it was of very brief duration and almost 

 immediately disappeared. 



Table VIL 



Giving the temperature change daily from 22nd to 30th September 

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





September 

 22. 



September 

 23. 



September 

 24. 



September 

 25. 



Assam ... ... 



+ 0-8° 



-10° 



-1.9« 



-20° 



North Bengal 



+ 3-0 



+ 1-2 



-2-8 



-2-0 



Bihar 



+ 2-2 



+ 1-5 



-0 3 



-►2.1 



United Provinces 



-2-0 



-O'l 



+ 1-2 



+ 0-5 



Punjab 



+ 0-5 



-08 



+ 0-6 



+ 0-5 



Srinagar, etc. 



-0-2 



+ 0*2 



-I'O 



+ 1-2 



1 



j 



September 

 26. 



September 

 27. 



September 



28. 



September 

 29. 



September 

 30. 



As am ... ... 



+ 0-5° 



-0-1° 



+ 2-8° 



+ 0-6° 



+ 0*2° 



North Bengal 



-1-4 



+ 2-9 



+ 0-3 



+ 0-9 



-0-3 



Bihar 



-2*1 



+ 16 



+ 0-4 



+ 0-7 



-07 



United Provinces ... 



+ 0-7 



-ro 



-0-6 



+ 1-0 



+ 8 



Punjab 



+ 0-3 



-0-6 



-0-7 



-0'3 



+ 0'3 



Srinagar, etc. 



+ 0-6 



+ 01 



-0-2 



+ 01 



-01 



