valley, and generally from the iipj)er Lake region westward 

 to the Pacific coast. 



Week ending June 10. — The temperature was normal in 

 southern Georgia, in Florida and on the immediate Gulf 

 coast. Throughout the Rocky Mountain and Plateau regions, 

 the central valleys and Lake region and in the Atlantic 

 coast districts northward of Georgia the mean temperature 

 was below the normal, the deficiency ranging from 6° to 9° 

 per day from the Missouri valley eastward to ISTew England. 

 ]^o appreciable amount of rain fell over the Southern States. 

 Showers giving from one-half to one inch of rainfall occurred 

 in the lower Ohio valley, lower Lake region. Middle Atlantic 

 States and ]Srew England. In the lower Missouri and cen- 

 tral Mississippi valleys and over the central portion of the 

 upper Lake region very heavy rains occurred. 



WeeJc ending June 17. — The mean temperature of the 

 week exceeded the normal over the northern part of the 

 upper Lake region, in southern Florida and from the west 

 Gulf coast northward to Canada. In all districts east of the 

 Mississippi River except the upper Lake region the week 

 was colder than usual. In the middle and northern Plateau 

 regions, the lower Lake region and from southern jSTew 

 England to I^orth Carolina the daily deficiency ranged from 

 6° to more than 12°. The rainfall was unusually heavy for 

 the season in northern California, Oregon and adjacent parts 

 of Washington and Idaho. East of the Rocky Mountains 

 the rainfall for the most part was below the average. How- 

 ever, portions of the central Gulf and Middle and South 

 Atlantic States, Lake region and upper Ohio, Missouri and 

 Red River of the ISTorth valleys received amounts in excess 

 of the normal, 



WeeJc ending June 2Jf. — The temperature was below the 

 normal in eastern and southern California, throughout the 

 Plateau and Rocky Mountain regions and on the immediate 

 middle and south Atlantic coasts. In the central valleys, 

 Lake region, New England and the northern portion of the 

 Middle Atlantic States the mean temperature was above the 

 normal, the average daily excess ranging from 3° to 6° over 

 the more northerly portions of these districts. In the South- 



