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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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