more than the average rainfall in the Atlantic coast districts 

 northward of Virginia. 



Week endiiKj June 11. — In the northern Rocky Mountain 

 region, and the middle and northern Plateau and Pacific 

 coast districts the week avemged cooler than usual. Over 

 the southeastern Kooky Mountain slope, the Missouri val- 

 ley, west Gulf States, and in all districts east of the Missis- 

 sippi River, except extreme southern Florida, the week was 

 warmer than usual. In the lower jSIissouri, central Missis- 

 sippi, and upper Ohio valleys and over most of the Lake 

 reirion, Middle Atlantic States, and New England, the 

 rainfall exceeded the average and in portions of all districts 

 named was very heavy. In the central Missouri and lower 

 Ohio valleys and generally throughout the Southern States 

 the precipitation was below the average. 



Week ending June 18. — The week averaged cooler than 

 usual over the interior of northern California, on the north 

 Pacitic coast, and in nearly all districts east of the Rocky 

 Mountains. The deficiency in temperature ranged from 3° to 

 6° per day, the most marked departures occurring in the cen- 

 tral Mississippi and lower Ohio valley's, the southern portion 

 of the Lake region, and the interior portions of the Middle 

 Atlantic States and New England. Generally throughout 

 the Atlantic coast districts, includinp; the upper Ohio valley 

 and the greater part ot the east (lulf States the rainfall was 

 much above the average. From the Gulf coast northward 

 to the Lake region the precipitation was much below the 

 average. 



Week ending June 25. — The week averaged warmer than 

 usual along the south Atlantic, Gulf, and Pacific coasts. 

 Over the eastern portion of the lower Lake region the aver- 

 age daily temperature for the week was nearly normal. 

 Elsewhere the week averaged cooler than usual, being de- 

 cidedly cool on the northern New England coast and from 

 the upper Ohio valley westward to the central and northern 

 Plateau regions. Throug-hout the central vallevs the aver- 



DO 



age daily temperature deficiency amounted to (5° or more, 

 and in the northern Rocky Mountain region and upper Mis- 

 souri valley it ranged from It^ to 12°. The rainfall was 



