1884.] 



of the Bay of Bengal in 1883. 



121 



As the rainfall was especially heavy in Orissa and the Central Pro- 

 vinces, I give the following table shewing the average district rainfall for 

 each day of the period (June 27th to July 3rd) in these two divisions of 

 the Empire, and illustrating more fully than the previous statement the 

 distribution of the rainfall in a portion of the area covered by the dis- 

 turbance. As daily returns of rainfall in Central India and the Bombay 

 Presidency are not at my disposal, I am not able to give the corresponding 

 data for the western portion of the course of the cyclone. 



Division. 



District. 





Orissa 



C hittasgarh 



Nagpore 



Nerbudda 



Jubbulpore *| 



Pooree 



Cuttack 



Balasore 



Sambalpore .. 



Raipore 



BUaspore 



Nagpur 



Bhandara .... 



Wardba 



Balaglaat 



Jubbulpore .... 



Sangor 



Damoh 



Seoni , 



Mandla 



Betul 



Chhindwara... 

 Hoshangabad 

 Nursinghpore 

 Nimar 



5 



5 



6 



5 



4 



1 



5 



3 



4 



4 



3 



4 



5 



3 



7 



7 



3 



5 



4 



3 



0-23 



0-06 



0-71 



0-32 



1-74 



Oil 



106 



2-81 



1-29 



1-21 



0-59 



0-46 



0-41 



0-83 



002 



0-55 



115 



101 



005 



0-06 



2-58 



303 



2-00 



0-31 



nil 



0-51 



1-48 



0-57 



0-01 



0-08 



013 



0-26 



0-04 



0-68 



0-20 



0-19 



0-37 



0-72 



0-68 



0-44 



6-15 



4-50 



2-66 



0-74 



0-73 



0-35 



0-19 



0-04 



nil. 



0-23 



1-44 



nil. 



nil. 



0-38 



0-04 



012 



nil. 



001 



015 



014 



1-83 



2-07 



302 



117 



1-30 



0-51 



nil. 



2-71 



1-82 



0-03 



0-54 



003 



0-26 



0-73 



0-26 



0-43 



103 



001 



0-88 



nil 



0-01 



nil. 



0-09 



1-05 



1-60 



0-56 



3-88 



2-99 



1-91 



2-47 



0-66 



0-28 



0-27 



2-76 



002 



3-91 



4-16 



2-90 



0-53 



0-64 



nil, 



nil 



0-09 



0-09 



nil. 



0-05 



2-25 



0-25 



nil. 



0-71 



0*02 



0-10 



0-07 



0-06 



nil. 



0-91 



0-06 



0-96 



019 



5-62 



0-06 



nil. 



013 



0-01 



001 



001 



001 



005 



0-01 



0-06 



0-02 



nil. 



nil. 



003 



nil. 



004 



nil. 



007 



nil. 



0-38 



10-86 

 9-66 

 8-70 

 3-69 

 5-38 

 2-05 

 8-87 

 9-42 

 5-04 

 4-79 

 3-40 

 113 

 1-05 

 5-47 

 0-54 

 615 

 6-77 

 5-68 

 2-48 

 7-28 



The chief peculiarity in the distribution of the rainfall was the con- 

 trast between the large amounts registered at stations to the south of the 



