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Mountain Snowfall Measurements

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Mountain Snowfall Measurements JANUARY, 1913. MONTHLY WEATHER REVIEW. 159 Frewo, Cal.: No unuwal phenomenon of this charact.er was observed 12. He states t,hat since two photographic-photometric until after November 10, 1912. On this date a very good general rain exposures on the constellation Coma Berenices, one on June occurred and cleared the atmosphere of the dust. which gives it a very hazy a pearance during the dry season. Duriiig tlie remainder of 12, of SO minutes, ancl the other on June 19, of 90 minutes, Novernger a number of very beautiful su1iset.s were observed. which failed to show stnrs revealed by an exposure of an hour differed from the usual phenonienon in that t.he brilliant. c:oloriiigs were on June 3, the disturbance in the atmosphere may have more widely and more evenly diffused than is conmion. Approxi- had its commencement between June 6 and 12. He mately 120° of the western horizon was colored, the hues reaching well t,oward t,he zenith aiid continuing with a brilliaiice more or less notice- estimated the decrease in atmospheric transmissibility at able for fully an hour after sunset. The dur:tt.ion was :tu especinl from 10 to 15 per cent. feature of the phenomenon. The reds were most conspicuous. but Observations from high Alpine peaks and from bal- other colors in that portion of the spectrum. t.he yellows aiid oranges, loons indicate that the haze was confined to great eared first in order, were not much less so. whichSanta e, N. Mex., December 29, 1912: The sunset glow this evening heights. It seems to have diminished greatly by Noveni- was especially"Y brilliant. By 5.10 p. m. tlie entire western sky was rosy ber, 1912, although some observers saw evidence of it at from llOo north to 90' sout,h of t,he sunset. pnint. and upward fully the end of the year. 65O. By 5.20 p. m. the colors had become brilliant red about t,he sunset Su.~n:m.a~y.-Theeruption of Katmai Volcano, on June point, shading off to a beautiful rosy red in t,lie distance. By 5.30 p. m. the lower COlOrS had become dark red and yery I)rilliniit,. There- 6, 1912, was followed bv a fall of volcanic ash over all of after the colors faded rapidly, and the last glow wns seen at 6.10 p. ni. southeastern Alaska a6d southward into the State of Washing ton. In the following lett,er, wluch is a reply to circular A hazy or smoky condition of the atmosphere that was letter of December 2S, 1912, abteiition is c.alled t,o the first observed in the United States from June 8 to 10, well-known fact that brilliant t,milight c.olors tire only but a parently did not reach its maximum intensity observed under favorable niet,eorological c,oiiclitioiis: until Yune 20 to 25, was also observed in Europe and During the summer of 1911 I epeiit, from June 12 until September 1 in northern Africa. In Euro e it was not generally in Prince Edward Island, Canada. Almost the entire summer there were brilliant pink sunsets that were very similar to those in tlie au- observed until after June 20, a7 t,hough there is evidence tumn of 1883. Previous experience in that region shows that brilliant that it may have been present previous to June 12. In afterglow sunsets may be expected in summer. Algeria, northern Africa, there is evidence that it was In 1912, from June 5 until September 7, I saw no aft,erglow t,hat was present as earl as June 19. brilliant, and only a few that were slightly reddish. The weather was unusually damp for the region all sunimer. Astronomicas observations, and especially astronom- It would appear that the amount of moisture must. have had some ical photography, together with pyrheliometric meas- relation to the absence of t.he afterglow of t,he sunsets in 1913 in t,he urements and records from sunshine recorders, indicate above region.-Prof. C. C. TROWBRIDGE,Department. of Physics, that the haze caused a marked decrease in atmospheric Columbia University, New York City. transparency. There seems to be good evidence that unusually biil- Twdight colors in the United States durin the fall of liant red sunsets were observed in the Unit,ed States dur- 1912 were more brilliant than usual and pera aps also of ing the fdof 1912, ancl espec.iallyin November, a.nd in bhe greater duration. The red shades were especially drier sections of the counttry, where condit,ions we,re pronounced. especially favorable for such observations. It does not At the end of 1912 the haziness appeared to be de- ap ear that the twilight colors have been markedly creasing. d&erent from t,Iiose of ot.lier years except for an increase in int,ensity, and in some cases an iiic.rease in duration. MOUNTAIN SNOWFALL MEASUREMENTS. While the purple or rose-colored glow t,liat hns been By BENJAMINC. RADEL.Local Forecaster. Weather Bureau. observed to overspre.ad the sky a short, time aft,er sunset or previous to sunrise lias been a proillinent featsureof As the irrigation systems of the country increase, the the displays, it lias not been comparable wit.li t,lie tift,er- need of more accurate measurements of the water supply glows observed in 1SS3.,. from the mountain snow fields becomes greater. An Atmospheric turbidity in. Europe i.n i9l$?.-The reader is experience of two years' actual work in the snow fields of referred to the scientific journals2 for details of the a portion of the Rio Grande National Forest in Mineral many observations that indicate decreased atmospheric County, Colo., at elevations exceeding 9,000 feet, has trans arenc in Europe during t'he latter part of 1912. demonstrated that the problem is not so complicated Near$ all tze writers fix the date of the first appearance as it may appear to the casual visitor to the mountains. of the haze between June 20 ancl 27; Dr. L. Steiner, The apparent confusion in the distribution of the snow however, finds evidence of uiiusually hazy conditions as layer, here the bare hillside, there the dee even layer early as May, 1912, which were intermittent, in character of the forest, and beyond the great timber [ne drifts, is, and appeared to be connecked with antic.yclonic weather upon closer RC uaintance, found to be the result of conditions. The intensity of the haze appeared to increase natural causes, 7t le most im lortant of which is the anole with each recurrence, until a maximum was attained in the slope, on which the snow Les, makes with the sun. In Jul . the high regions of the mountains the sun shines for a & his reply to circular letter of December 28, 1913, greater number of hours during the winter than at lower Dr. Adolf Hn atek, of the Vienna Astronomical Observa tory, elevatioiis because the sky is less frequently obscured by places the first appearance of the haze previous to June cloud, and the sun's rays are also stronger, because they 1 The eruption of Krakatoa and subsequent phenotuena. Report of the Krakotoa Marten, W. SchwLhung ron Sonuenstrahung und Sonnenscheindauerdmcli eine commit.tee of the Royal Soriet.y, p. 340. and frontispiece. atmosplLirische Triihuug iru Sommer 1912. Met. &it. Nov.. 191%Bd. 29. p. 533. Wolf, bf. Triibung der Atmosphiire uud Diimnieruugsersclieinllligen. Net. Zeit., lin8chizilz.I_ Ion. Paul. Triihuuedes Hirnrnels in Siidt.;rol. Met. Zeit..,, Nov.. 1912. Bd. July 1912 Bd. 29 p. 339. 29, p. 534. Bhseh, %r. Eihe neue optische Storung in der .4tmosphLire. Met..Zeit., Aug., 1912, de Qnmuoin. Dr. -4. Nerkwiirdiger Hirnmplsanhlick im Inneren Groulands im Som- Bd. 29 p. 385. mer 1912. Met. Zeit.. Der. 1912. Bd. "9 W. Mat& J. A4tmosph&rischeTriibun Yet Zeit.. 191'' Bd. 29, p. 385, %fi. Hdlmaiia. 0. Diebrsache der uug&&lirhen Triibung der Atmosphtire im Sommer Hildebr&Lwon, H. H. Atmospharisc%e Triibuug in &weden. Met. Zeit., Sept.., 1912. Met. Zeit.. Jan., 1913, Bd. 30, 34. 1912, Bd. 29, p. 442. Sfrincr, lir. L. Zur atmosphkirisckm Triibung im Sommer 1913. Yet. Zeit., Jan., Stentrel, A. Die neue Diimmerungsstorung. Met. Zeit.. Ort., 1912. Bd. 211, p. 485. 1913 Bd. 30 p. 30. Hahn. F. Die atmcspharische Storungim Sommer 1913. Met. Zeit., Oct., 1912, Bd. S/hio, W.'N. Peculiar appearance of the sky during the summer, 1912. Qr.J. R. "9#. pse. Met. 6oc. Oct.. 1912 v. 38, p. 312. ergand, Albert. Die anomale Triibung der Atmosphiire. Met. Zeit., Nov., 1912, JeRpen 'Dr. Chr. 'Uber die grosse atmospharisch-optishe Storung von 1912. Re- Bd. !29, p. 532. print from Mitteil. d. Vereinig. v. Freunden d. Astron. u. kosm. Physik, Berlin. Unauthenticated | Downloaded 09/25/21 11:51 PM UTC 160 MONTHLY WEATHER REVIEW. JANUARY,1913 shine through a rarer atmosphere. Actual measurements In order to measure the water value of a given snow show that on south slopes the main body of tlie snow layer it is required to know both the depth and the density generally melts within a few days after it falls, even of tlie layer. The accepted method of measuring the though thermometers exposed a few feet above the depth is by means of snow scales, permanently fixed, ground show temperatures well below the freezing point. from which the depth niay be read at any time. The Prom the fact that the main body of the snow that falls scale should be as small in cross section as practicable, so on south slopes disa ears time and again during tlie as to reduce reflected heat and consequent melting of t,he course of a winter, wPi 11 e at the same time the mountain snow imiiiediahely about it,, and at the same time it must streams continue at low stag!, it seems ressonable to be large enough for graduations that may be read at some conclude that the greater portion of the snow that falls distance, say 25 feet or more.
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