SCIENCE ROOM ^Cm> FEB \i ''pljilJII^TUWlS OF Oregon's climate, If FOR THE FOREST INDUSTRY SEPTEMBER I960 CLIMATOLOGICAL NOTE NUMBER 32 FREQUENCIES OF AMOUNTS OF DAILY PRECIPITATION IN CENTRAL OREGON (CHEMULT, CRATER LAKE, FREMONT, REDMOND) Question: "During a given 10-day period in Central Oregon, what is the likelihood that precipitation during a day will be light, medium, or heavy?" Table: As an example of how to read the Table, look at the top row of numbers for the period 1-10 January. The values tabulated are based on actual observations made at the stations indicated during the years 1949-58, and are presented on the basis of "days in 100 days". The numbers 0, 1, 2, and 3 above the columns stand for amount of precipitation as follows: 0 no precipitation 1 light precipitation Trace through 0.09 inch 2 medium precipitation 0.1 through 0.49 inch 3 heavy precipitation more than 0.49 inch That is, during the first third of January at Chemult, rainless days have occurred at the rate of 43 days in 100 days, and light precipitation has fallen at the rate of 17 days in 100 days. Combining these two statements, precipi tation at Chemult during the period has been either absent or light on 43+17, or 60 days in 100 days. This last value for Crater Lake is 32+16, or 48 days in 100 days, and at Fremont, it is 66+21, or 87 days in 100 days. Conversely, at Fremont precipitation rate has been medium or heavy on 100 - 87, or 13 days in 100 days during the first third of January. Similar combinations of data may be made with respect to various intensities of precipitation at other times of the year. The data: Because of the nature of precipitation, tabulations here cannot be considered any more than a suggestion of patterns in time and space of precipitation occurring on a given day in Central Oregon. Note that "precipitation" includes rain, snow, hail, and sleet expressed in terms of water equivalent. Similar data for Klamath Falls and Medford are available in detail as Climatological Notes 10 and 16 of this series. • William P. 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