Orologists Will Be in Attendance. It Is Both Important and Desirable That

Orologists Will Be in Attendance. It Is Both Important and Desirable That

orologists will be in attendance. A. Fleming, General Secretary, Am- It is both important and desirable erican Geophysical Union, Depart- that American meteorologists assume ment of Terrestrial Magnetism, 5241 their full share in contributing to the Broad Branch Road, N. W., Washing- expenses of this meeting. I should ton, D. C., or, if preferred, they may like therefore to appeal to all mem- be sent direct to the undersigned.— bers of the American Meteorological W. R. Gregg. Member, Finance Com- Society to have a part in this note- mittee, American Geophysical Union, worthy undertaking. Contributions, (c/o U. S. Weather Bureau, Washing- or pledges, should be sent to Dr. John ton) . The Terms of Meisinger Award Announced The committee on the Meisinger ments of contestants, preference will Aerological Research Fund award, be given, other things being approx- appointed by President Gregg, in imately equal, to meritorious efforts of the younger students and workers in accordance with a vote of the Council, meteorology. announces the following terms gov- 3. Studies having for their purpose erning an award from the income of the application of free-air data to the Meisinger Fund:— forecasting problems are specially recommended, this being the line along "That the Society make an award which Dr. Meisinger was principally of $100 or awards totalling at least this amount, together with suitable engaged; but any other topics in the certificates or plaques, under the Mei- field of aerology are admissible. singer Aerological Research Fund at 4. The committee will consider dis- the Annual Meeting in December 1938 cussions of aerological subjects pre- for one or more particularly meritori- sented at a meeting of a scientific so- ous and outstanding research con- ciety or published. tributions in aerology, either theo- 5. The period in which these papers retical or applied. shall have been presented or published "The following terms and conditions must be that from December 27, 1937' are stipulated: to November 30, 1938, inclusive. 1. The award is open only to citizens C. F. Brooks, chairman of countries in the Western Hemi- W. R. Gregg, ex-officio sphere. D. M. Little 2. Although no restrictions are E. J. Minser named as to age or scientific attain- C.-G. Rossby (Committee.) 4 Bibliography Prepared by Mr. Richmond T. Zoch, Librarian, U. S. Weather Bureau (Continued from Oct. 1937, BULLETIN, p. SUU) QUARTERLY JOURNAL OF THE ROYAL a contribution, pp. 85-95.—A. Walter: The METEOROLOGICAL SOCIETY, v. 6U, no. 273, climate of British East Africa, pp. 97-116.— January, 193S: Editorial, pp. 1-2B.—T. E. W. R. H. Weightman : The cyclone series in the Schumann: The theory of hailstone forma- Caribbean Sea, October 17-24, 1935, pp. 117- tion, pp. 3-21.—I. D. Margary: Report on the 119.—v. <U, no. 275, April, 1938: F. J. W. phenological observations in the British Isles Whipple: Modern views on atmospheric elec- from December, 1935, to November, 1936, pp. tricity, pp. 199-213.—E. W. Barlow and S. 21-22— H. Fairfield Smith: Report of a pre- Chapman: The auroral display of January liminary statistical investigation of flowering 25-26, 1938, pp. 215-221.—G. S. Callendar: The dates of plants recorded in the Phenological artificial production of carbon dioxide and its Reports of the Royal Meteorological Society, influence on temperature, pp. 223-240.—R. A. pp. 23-46.—C. W. B. Normand: On instab- Hamilton: The Oxford expedition to North ility from water vapour, pp. 47-70.—C. W. B. East Land, 1935-36. General meteorology, pp. Normand: Kinetic energy liberated in an 241-252.—G -Manley: Meteorological observa- unstable layer, pp. 71-74.—C. S. Durst and R. tions of the British East Greenland Expedition, C. Sutcliffe: The importance of vertical mo- 1935-36, at Kangerdlugssuak, 68° lo' N, 31° 44' tion in the development of tropical revolving W, pp. 253-276.—R. M. Poulter: Cloud fore- storms, pp. 75-84.—C. J. Boyden: The mech- casting: the daily use of the tephigram, pp. anics of the depression: Some criticisms and 277-292.—S. K. Banerji: Does thunderstorm Unauthenticated | Downloaded 10/01/21 08:32 PM UTC rain play any part in the replenishment of the Kans., 1935-36, pp. 388-92.—J. H. Gallenne: earth's negative charge? pp. 293-299.—J. Disturbance in the Gulf of Mexico, November Bjerknes: Saturated-adiabetic ascent of air 23-26, 1937, pp. 392-3.—Bibliog., obs. and through dry-adiabatically descending environ- tables, pp. 398-410.—December, 1937: W. R. ment, pp. 325-330.—R. Bureau: Centres of Gregg and I. R. Tannehill: International thunderstorms and "centres" of sources of at- standard profections for meteorolopical charts, mospherics, pp. 331-335. pp. 411-15.—Irving F. Hand: Review of United States Weather Bureau solar radiation inves- MONTHLY WEATHER REVIEW, August, tibations, pp. 415-41.—E. H. Fletcher: Floods 1937: Raymond Price and Robert B. Evans: in the Sacramento Valley, Calif., December Climate of the West Front of the Wasatch Pla- 1937, pp. 441-44.—J. P. Kohler: Preliminary teau in Central Utah, pp. 291-301.—Edgar W. report on tornadoes in the United States dur- Woolard: The geometric theory of halos, V, ing 1937, pp. 445-6.—Willis E. Hurd: North pp. 301-2.—Willis E. Hurd: Tropical disturb- Atlantic tropical disturbances of 1937, p. 446. ances on the North Atlantic Ocean, August, —Bibliog., obs. and tables, pp. 447-68.— 1937, pp. 303-4.—Bibliog., obs. and tables, p. January, 1938: Richmond T. Zoch: A brief 304-321.— September, 1937: Elsasser, W. M.: list of works on meteorology, pp. 1-3.—B. C. On some properties of the water-vapor spec- Haynes: Upper wind forecasting, pp. 4-6.— trum and their relations to atmospheric ra- Adalberto Serra and Leandro Ratisbonna: Air diation, pp. 323-326.—William H. Wenstrom: masses of southern Brazil, pp. 6-8.—R. J. On pilot balloons and sources of light for high Martin: Duststorms of May-December 1937 altitude upper-wind observations, pp. 326-331. in the United States, pp. 9-12.—J. P. Kohler : —Willis E. Hurd: Tropical disturbances on Weather of 1937 in the United States, pp. 12- the North Atlantic Ocean and the Gulf of 14.—George W. Mindling : Note on early tor- Mexico, September 1937, pp. 332-335.—Pat J. nadoes in Georgia, p. 14.—Bibliog., obs. and Harney: Note on H. C. Huang's Investigations tables, pp. 15-33 .—February, 1938: W. J. of Frontogenesis in the North Pacific, pp. Humphreys: Springs that mysteriously ebb 335-37.—Charles M. Lennahan: Monthly ob- and flow, p. 35.—Bertram E. Hall: Geography served sunspot relative numbers for the pe- and rainfall of the Nebraska sandhills, pp. riod 1920-26, inclusive, p. 338 — Bibliog., obs. 36-38.—Giles Slocum: The normal temperature and tables, pp. 338-57.—October, 1937: Herbert distribution of the surface water of the west- Lyman: Serial numbers of weather bureau ern North Atlantic Ocean, pp. 39-43.—Charles publications, pp. 359-63.—Charles M. Heck: M. Lennahan: The effect of the magnetic Preliminary report on observations of air cells storm, January 22-26, 1938, on telegraphic in snowflakes and in other forms of ice, p. transmission, p. 43.—Willis E. Hurd: Auroras 364.—Thomas R. Reed: Further observations of January 21-22 and 25-26, 1938, pp. 43-44.— on the North American high-level anticyclone, Bibliog., obs. and tables, pp. 44-62.—March, pp. 364-66.—Bibliog., obs. and tables, pp. 1938: Horace R. Byers : On the thermodyna- 367-83.—November, 1937: Willis R. Gregg: Ad- mic interpretation of isentropic charts, pp. vances in international meteorology in 1936 63-68.—W. R. Stevens: Relation of pressure and 1937, pp. 385-387.—W. J. Humphreys: tendencies to cyclones and fronts, pp, 68-70.— A curious photographic cloud effect, pp. 387. Earl C. Thom: Temperature changes in North —A. D. Robb: Comparison of temperatures and South Carolina, pp. 70-73.—Bibliog., obs. from roof and ground exposures at Topeka, and tables, pp. 74-91. (To be c -4{ Corrigenda March, 1938, BULLETIN, p. 125, in heaters in use were designed as 2nd paragraph of the note on "Orchard smudge pots, at a time when smoke was considered desirable, so the Heating .. .", last line, for "$60,000" smudge nuisance is now acute when- read instead "$60,000,000". This er- ever there is a succession of cold ratum gave an unfortunately errone- nights". ous impression, in regard to which J. March, 1938, BULLETIN, p. 109, the B. Kincer writes: aerological data on which the curves "In fact 'smudging' was discarded in Figures 1 and 2 are drawn was in- years ago instead of the growers correctly copied or transmitted. The "gradually adopting heating". During following significant points should be the 1937 freeze about 82 million gal- lons of oil were burned, costing$4,000,- changed or inserted: in Fig. 1, Fair- 000 for the oil alone. With a saving banks ascent, at 1050 m the tempera- of only $60,000 as published, this ture was —4°, at 1450 m —4°, at would certainly be a 'losing game'. As 2550 m —10°; the Miami ascent, at a matter of fact the saving was ac- tually several times the cost of the 3420 m should be 3°; the Fort Smith entire operation, including that of the ascent at 2350 m was —24°, and at oil." 3500 m —28°. In Fig. 2, Omaha as- However in regard to smudging vs cent, at 3380 m the specific humidity heating, F. A. Brooks of the Califor- nia Agric. Experiment Station, writes was 2.1 g. that: "Unfortunately, most of the Unauthenticated | Downloaded 10/01/21 08:32 PM UTC.

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