close to the nor< as it recedes from the Bay 



an average of 82" at Kaliaganj, uhich comes very much urnler tin- 

 influence of the Himalaya. Tn this northern belt the fall rapidly 

 slackens towards Darbhanga and Muzaffarpur, but again in. iv.isi's 

 iins in the north of Champaran. Owing 





■m-j.t.'d ! 



the Southern tract. and jimha N\ I lie next highest rainfall to L'urneali, 



hhanj, which attain 3550 ft. at Meghasani. There is, however, no 



meteorological station cither here ,,;■ (in f'arasuath, the highest 



!y regularly graded 

 i recording stations 



is a general average decreas 

 to more exceptions. Not 



