Nevada County CA Archives History - Books .....Meteorolgy 1867 ************************************************ Copyright. All rights reserved. http://www.rootsweb.com/~usgenweb/copyright.htm http://www.rootsweb.com/~usgenweb/ca/cafiles.htm ************************************************ File contributed for use in USGenWeb Archives by: Joy Fisher sdgenweb@yahoo.com December 5, 2005, 4:07 pm Book Title: Bean’s History And Directory Of Nevada County, California METEOROLOGY. The subject of my sketch, having every altitude from /a few feet to eight thousand above the ocean level, must necessarily have a variety of climate. Near the plains frost is rare, while at Meadow Lake scarcely a night passes without leaving traces of frost in the morning. In the upper part of the county snow, if not Winter, reigns one-half the year; while a snow fall at Rough and Ready and below is an uncommon occurrence. The fall of snow is light over that portion of the surface of the county having an altitude of 2,500 feet or less. At Nevada City, which has an elevation of about 2,350 feet, it rarely falls to the depth of two feet, and it seldom lies on the ground more than two or three days. Sleighing about Nevada and Grass Valley is not persisted in beyond a few hours, the ground never freezing so as to give a sound base for the snow to rest on for that purpose. At Bear Valley, snow fell during the Winter of 1858-59, twenty-four feet, by actual measurement, falling on April 19th of that season eighteen feet deep. Further up, in the region of Meadow Lake, the fall is heavier and the Winters more severe. But, the Winter in any part of Nevada county is not so cold by far as in the same latitude on the eastern side of the continent. This is due, to a large extent to the latent heat set free by the condensation of the vapors on our mountains which come from the South Pacific ocean. The sun, during our rainy season, pours down his ferved rays upon the Southern hemisphere, which is largely of ocean, and an immense amount of moisture is taken to the clouds which, borne along by the southeast trade-winds till transferred to the southwest trades, are driven against the Sierra Nevada chain of mountains. The cold of the elevated region condenses the moisture into rain or snow, and the heat borrowed in a latent state in the South Pacific is set free to ameliorate our Winter climate. From a few observations it would seem that some parts of the county are subject to heavier falls of rain than other parts, and the rain fall of the county is much heavier than in the valley regions of the State. I am indebted to James Whartenby, Esq., who has kept a rain-guage at the office of the South Yuba Canal Company, in Nevada City, and, also, a thermometrical register, during many years, for interesting facts. The destructive fires that have so frequently visited Nevada, have consumed some of the journals of Mr. Whartenby, but what have been spared will serve to give some idea of the climatic changes experienced in the county/particularly in the central part, that portion having an altitude of from two thousand to three thousand feet. From these journals it appears that during the rainy season of 1861-62 the fall of water was 109 inches; 1862-63, 27.87 inches; 1863-64, 17.26 inches; 1864-65, 54.49 inches; 1865-66, 59.26 inches. That part of the rainy season of 1866-67, ending on the 1st of January, 1867, was extraordinary, for the amount of water fallen; 42.39 inches are reported at the office of the Canal Company. Mr. Whartenby estimates the average rain fall since the settlement of the county by Americans, at from fifty to fifty-five inches. The above figures have been called in question heretofore as being too large, and it has been supposed that the rain-guage kept at Nevada could not be correct. To settle the question, Mr. Whartenby has had a new guage made by Tennent, of San Francisco, and the tests show the new guage to give rather more water than the old one, both standing side by side. The figures above are, therefore, too small. It is proper to remark that the rain fall here is not unusual, the mean annual fall on the globe being estimated at sixty inches, and in the northern hemisphere at about ninety inches. In the tropics of the eastern continent it is computed at seventy-seven, and in the western tropics at one hundred and fifteen inches. The latter is about the fall at Nevada City during the rainy season of 1861-62. But there are other places on the globe subject to still greater deluges from the clouds. According to Maury, rain fell at Paramaribo, in South America, in one season, to the depth of two hundred and twenty-nine inches, or nineteen feet. Brazil has had a rain fall in a season of twenty-three feet, and twenty-five feet have fallen in a year at South Bombay. In forty-one days a hundred and fifty-three inches, or thirteen feet of water fell on the west coast of Patagonia. From the facts before us, it is safe to say that the fall of rain annually in Nevada county is not above the average on the surface of the globe. A late fall of snow occurred at Nevada and Grass Valley May 21,1861, which broke down and damaged fruit trees. It was very moist and heavy and in a few hours was dissolved in water and gone. It has been observed by those in the employ of the South Yuba Canal Company, that when the thermometer at Nevada is at 37° to 38° Fahrenheit, snow falls instead of rain. If the thermometer shows 43° to 44° it rains further on about twenty miles above Nevada, and snows beyond. At 50° to 51° it rains to the summit. These observations apply, of course, to times when vapors of the clouds are condensing in the form of rain or snow. We can give only some general idea of the changes in the thermometer as observed at the office of the South Yuba Canal Company. The coldest day was January 20, 1854, when at seven in the morning the mercury stood at 1° above zero, while the hottest day ever known at the same, point was 142 1/2° in the sun. For extraordinary changes of weather, the fact may be cited, that on April 12, 1859, the thermometer indicated at 2 1/2 o'clock P. M., 94°; seven and a half hours later, at 10 o'clock, the mercury had fallen to 27°. The temperature in the Winter season, in the morning, ranges from 12° to 40°, and in Summer, the hottest weather in the sun is usually from 110° to 130°. These remarks are only intended to show the extraordinary extremes of heat and cold. Generally Nevada county has a pleasant and equable climate; in fact, all who have enjoyed it for a time are captivated, and if away, long to return to it again. The Summers are all sunshine and are quite warm, but the nights are cool and refreshing inducing sound and invigorating sleep, while the Winters are not severe except at the highest altitudes, and even there the degrees of cold are not to be estimated by the depth of the snow. A large number of persons and some families passed the Winter of 1865—66, very pleasantly at Meadow Lake, and while this volume is going through the press, a great many more are following the example of their predecessors. Additional Comments: Extracted from: Bean’s History and Directory of Nevada County, California CONTAINING A COMPLETE HISTORY OF THE COUNTY, WITH SKETCHES OF THE VARIOUS TOWNS AND MINING CAMPS, THE NAMES AND OCCUPATION OF RESIDENTS; ALSO, FULL STATISTICS OF MINING AND ALL OTHER INDUSTRIAL RESOURCES. COMPILED BY EDWIN F. BEAN. PRINTED AT THE DAILY GAZETTE BOOK AND JOB OFFICE, 1867. File at: http://ftp.rootsweb.com/pub/usgenweb/ca/nevada/history/1867/beanshis/meteorol73gms.txt This file has been created by a form at http://www.genrecords.org/cafiles/ File size: 7.7 Kb