[Extract from the papers of the Chicago Meteorological Congress, August, 1893.] 1.-THE CONNECTION OF THE ARMY MEDICAL DEPARTMENT WITH THE DEVELOPMENT OF METEOROLOGY IN THE UNITED STATES. Maj. Charles Smart, U. S. A. Meteorological science in the United States was conceived and brought forth by the Army Medical Department. It was nurtured carefully as well in the then unknown West as in the East, and it gained strength year by year. Its progress was occasionally an- nounced from the office of the Surgeon General of the Army by such men as Forry, Espy, and Coolidge, and when it attained its maturity and was able to work its own way in the world, it was to one, once a member of the Army Medical Department, that it owed its establish- ment in its present prosperous line of business. The Weather Ser- vice of the United States may well be said to be the child of the Army Medical Department. Gen. Joseph Lovell, the first Surgeon General of the Army, ap- pointed in 1818, is usually credited with the honor of having insti- tuted the Army Meteorological Service, although some of the credit is diverted to the then Secretary of War, the Hon. J. C. Calhoun, be- cause he approved of the rules submitted by the Surgeon General, and so gave them the force of law. In urging the approval of the rule requiring a diary of the weather to be kept, Surg. Gen. Lovell re- marked that " Every physician who makes a science of his profes- sion or arrives at eminence in it will keep a journal of this nature, as the influence of weather and climate upon diseases, especially epidemic, is perfectly well known. From the circumstances of the soldier, their effects upon diseases of the Army are peculiarly interesting, as by proper management they may in a great measure be obviated. To this end every surgeon should be furnished with a good thermometer, and in addition to a diary of the weather, should note everything relative to the topography of his station, the climate, complaints prevalent in the vicinity, etc., that may tend to discover the causes of diseases, to the promotion of health, and the improvement of medical science." Every reference to the subject published from the office of the Surgeon General gives credit to Dr. Lovell. In one of the volumes of meteorological tables it is stated, for instance, that " In 1819 a system of meteorological observations was commenced and zealously pro- moted by Surg. Gen. Joseph Lovell. The unpublished records extend to 1820." Even Surg. T. G. Mower, who, in 1843, read a paper at the 2 centennial anniversary of the American Philosophical Society on the connection of the Army Medical Department with meteorological science, states positively that during the year 1818 the surgeons at military posts were directed to keep regular records of the weather and transmit them quarterly to the Medical Bureau at Washington and that the earliest registers thus transmitted and on file in the Surgeon General's Office are dated January, 1819. Nevertheless it appears that Surg. Gen. Lovell's credit must be restricted to the fact that he appreciated the value of the existing rules of the Medical Department, in regard to meteorological observa- tions, and continued them instead of dropping them out, as he might have done. The earliest meteorological journal on file in the office of the Surgeon General, instead of bearing date January, 1819, is dated at Cambridge, Mass., July, 1816. On its first page is written the fol- lowing : Among the rules for the medical staff of the Army of the United States is that which makesit the duty of each hospital surgeon and director of a department "to keep a diary of the weather, together with an account of the medical topography of the coun- try in which he serves." Wherefore the following sketch of Boston and its vicinity, and particularly of Charlestown, is offered to the commander in chief, Maj. Gen. Brown, by Benjamin Waterhouse, M. D., hospital surgeon and director of Department No. 2, Northern Division, as a first step in fulfilling this desideratum. Cambridge, July, 1816. From this introductory sentence the inference is warranted that this meteorological report was a new thing to Dr. Waterhouse, and that no doubt it was the first of the kind that he had submitted. In going back through the Military Laws, Rules, and Regulations of the United States, an order may be found, dated May 2,1814, which makes it a duty of hospital surgeons to keep a diary of the weather. Prior to this date neither the regulations of the Army nor the rules of the Medical Department made any reference to such a duty. Dr. James Tilton, of Delaware, was then the Physician and Surgeon General of the Army. He had been appointed in 1812 on account of his record as a hospital surgeon during the Revolutionary war and of his pub- lished views on hospital organization, which had been presented to Congress at the close of that war. As the order directing the keeping of a diary of the weather was issued during his administration, the credit of originating it belongs officially to him. He was occupied at the time on the northern frontier looking after the interests of the sick and wounded. The battles of Chippewa, Bridgewater, and Platts- burg took place during this summer, and one would have supposed that Army medical officers would have had more urgent matters to attend to than the observation of the weather; but when it is con- sidered that Tilton had devoted much of his life to the organization and administration of hospitals, and that only hospital surgeons and those elevated to the position of medical directors were called upon 3 to make the observations, there seems to be little doubt that the credit of instituting meteorological records at our permanent posts and hospitals should belong actually as well as officially to this officer. The meteorological journal, to which the topographical remarks of Dr. Waterhouse form an introduction, gives three observations daily, 7 a. m., and 2 and 9 p. m., on the barometer, thermometer, face of sky, and winds, with a column for remarks. The condition of the sky is indicated by hieroglyphics, such as Q fair, mostly fair, -== few clouds, ZZZ mostly cloudy, = = cloudy, rain, £ snow, and the force of the wind by a numerical exponent to the letters in- dicating direction, thus SW2. The regulations of the Medical Department issued in 1818, imme- diately after the appointment of Dr. Lovell as Surgeon General of the Army, spoke thus of the duties of a hospital surgeon : " He shall keep a diary of the weather in the form and manner prescribed, noting everything of importance relating to the medical topography of his station, the climate, complaints prevalent in the vicinity," etc. Of an assistant surgeon: "He shall make the proper*entries in the book containing the diary of the weather." Of a regimental sur- geon : " He shall observe all the regulations given for the surgeon attending a general hospital in relation to * * * the book con- taining a diary of the weather, the medical topography of his post or station, etc.; and if both the regimental mates be present the senior shall see that the diary of the weather be properly kept." Of a post surgeon : " He shall observe all the regulations given for a sur- geon attending a general hospital in respect to the books to be kept." It seems, therefore, that although Dr. Tilton instituted the records, the circumstances attending the war with Great Britain prevented an efficient compliance with the requirements of his order of May 2, 1814, and it was left to Dr. Lovell, favored by a prolonged period of peace and prosperity, to take up the suggestion and develop its use- fulness. In 1826 the first results of the work of the Army Medical Depart- ment in this direction were given to the world in a volume entitled " Meteorological Register for the years 1822-25, inclusive, from ob- servations made by the surgeons of the Army at the military posts of the United States; prepared under the direction of Joseph Lovell, M. D., Surgeon General of the U. S. Army, Washington, 1826." The meteorological tables in this volume were intended as a contribution and stimulus to the solution of the question whether, in a series of years, there is any material change in the climate of a country and, if so, how far it depends upon the cultivation of the soil, density of population, etc.; for at the time of publication contradictory opin- ions were held, some contending that as population increased and 4 civilization extended the climate became warmer, others that it be- came colder, and others again that there was no change. The military posts from which observations were given numbered 18, including Washington, and were situated between N. 27° 57' and N. 46° 39' and W. 67° 04' and W. 95° 43'. Fort Snelling, near the junction of the St. Peters and the Mississippi rivers, was the extreme northern and Cantonment Clinch, near Pensacola, the extreme southern station. The posts having the highest elevation were Council Bluffs, believed to be about 800 feet, and Fort Snelling, about 780 feet above the sea level. The observations from all the posts were arranged in monthly tables with a consolidation for each year and a similar consolidation for the whole period. The latitude and longitude of each place of observation were given, the mean temperature at 7 a. m., 2 and 9 p. m., the aggregate of mean temperature, the highest and lowest degrees and the range, the wind expressed in days of prevalence from each of 8 different points of the compass, and the weather in days of fairness, cloudiness, rain or snow. It was the in- tention, if similar observations could be obtained for eight or ten years, to collect such as had been made at an early period of the settlement of the country and to ascertain what changes had taken place in the Atlantic States, either in the mean temperature, the range of the thermometer, the winds, or the weather. The next publication was much more elaborate and embodied the data of the first volume by way of an appendix, in order to present the whole of the observations at one view. " Meteorological Register for the years 1826-30, from observations made by the surgeons of the Army and others at the military posts of the United States, pre- pared under the direction of Thomas Lawson, M. D., Surgeon General, U. S. Army. Philadelphia, 1840. To which is appended the Meteoro- logical Register for the years 1822-25 , compiled, etc. (published for the use of the Medical Officers of the Army)." The tables in the record for 1826-30 were similar to those in the previous publication to permit of comparison and consolidation. The compilation and able discussion of the results presented in this volume were the work of Assistant Surg. Samuel Forry, U. S. Army. For the better presen- tation of the observed facts the country was divided into a northern, middle, and southern division. In the first, on the sea coast of New England, the influence of the ocean was found to modify the range of the thermometer and the mean temperature of the seasons. In the interior of New York the range increased and the seasons were vio- lently contrasted. Further west near the Great Lakes a climate sim- ilar to that of the seaboard was again found; and in the interior beyond them extreme ranges became the rule. For example, the mean temperature of Atlantic and interior posts in the same latitude was found to be the same, but in the East that of winter was 6.05r 5 higher, of spring 4.13° lower, of summer 8.71° lower, and of autumn 0.40° higher than in the West; and the influence of altitude was ex- cluded from the observations which gave these results. The influence of the ocean was expressed also by the fact that the number of wet or foggy days on the New England coast was one-half greater than in the interior. Similar contrasts in the seasons and weather were discovered also in comparing the Lake posts with those beyond. The posts selected were Forts Brady, Mackinac, and Snelling, from 575 to 780 feet above the sea level. In the middle division similar laws were found to pre- vail. The seasons grew less uniform as the West was penetrated. Washington City and Fortress Monroe showed less difference between the mean temperature of summer and winter than Jefferson Barracks or Fort Gibson. In the southern division, bounded by the Gulf of Mexico, the seasons glided imperceptibly into each other, showing no great extremes. Thus, the difference between the mean temperature of the warmest and coldest month at Cantonment Brooke, in Florida, was only 17.68°, while that at Fort Snelling was 61.18°. It was developed further that the extremes of heat and cold did not occur at our most southern and northern posts, as these were situated on large bodies of water which exercised a modifying influence. Brady had a more equable climate than Snelling, and the mean summer temperature of Augusta, Ga., was greater than at the Florida posts. Lastly, it was discovered that the summer of a southern post differs from that of a northern one rather in its duration than in its inten- sity. In fact, the isotheral, isocheimal, and isothermal lines as far west as Fort Shelling became pretty well defined by a study of the observations thus far recorded. The prominent features of the cli- mate of the country having been thus outlined, it was expected that a continuance of the observations would in course of time permit of the composition of a complete meteorological chart. To this end the Surgeon General procured from Europe a number of Daniell's hygrom- eters for use at the more important stations, and De Witt's conical rain gauge was furnished to those posts not already provided with this instrument. About the same time was published a " Statistical report on the sickness and mortality in the Army of the United States, compiled from the records of the Surgeon General's and Adjutant General's Offices, embracing a period of twenty years, from January, 1819, to January, 1839, prepared under the direction of Thomas Lawson, M. D., Surgeon General, Washington, 1840." This work defined the sanitary conditions of each of the posts, detailed the more important incidents of their medical history, and concluded with a discussion on the relationship of climate and its seasonal differences to mor- tality, and the prevalence of such diseases as fevers, diarrhoeas, 6 catarrhs, and pulmonary diseases, rheumatism, etc. Two years later Forry republished the matter of his meteorological and statistical reports as a work on "The climate of the United States and its endemic influences." New York, 1842. 8°. When Dr. Forry resigned in 1840 Mr. J. P. Espy became attached to the Surgeon General's Office to collate the meteorological journals and study the steadily accumulating mass of facts. This gentleman, an enthusiast in meteorological science, was already well known by his book " On the Philosophy of Storms." He immediately sent out a circular letter urging the keeping of meteorological journals by vol- untary observers throughout the country, by colleges, high schools, naval and lighthouse stations, etc., on the forms prescribed for the Medical Department of the Army, especially requesting co-operation in his efforts to develop the phases of storms. By charting on skeleton maps the observations taken as a storm was passing he expected to determine its shape and size, whether round or oblong, and if the latter, whether it moved side foremost, end foremost, or obliquely, its velocity and direction, together with the direction of the wind at and beyond its borders, the barometric and ther- mometric changes accompanying it, and the extent to which such changes were felt. In 1843 he received journals from 50 observers who noted barometer changes and from 60 others who had no barom- eter, and in the preparation of his First Report to the Surgeon Gen- eral of the Army he utilized the observations of the months of Jan- uary, February, and March of that year. Twenty-nine beautifully engraved charts accompanied his report and illustrated the weather of the three months. On these charts the direction and length of the arrows showed the direction and force of the wind, the points being near the places of observation. The rain or snow fall was indicated by figures in red. A long black line represented the various maxima of pressure as shown by the barometer and a long red line the various minima. In brief, his deductions were that storms travel from west to east and have a central line of minimum pressure often of great length and at right angles to the direction of its advance. The storm in fact crosses the country like a line of battle, sometimes nearly straight, but generally with a convexity eastward at some point as if an impulse was carrying it forward there at a greater rate than the average of 36 miles an hour. The wind sweeps inward from all directions toward the storm center, its force and the extent of the disturbance around the line of diminished pressure being proportioned to the suddenness and magnitude of the barometric fall; when the latter is great the disturbance may extend for hundreds of miles, and is always accompanied by rain or snow. Fluctuations are greater at the north than at the south. During the passage of a storm the wind passes from easterly to westerly by way 7 of the north in the northern parts of the country, by way of the south in the southern parts. Storms usually begin in the far west beyond the sphere of the observations then made. Meanwhile the area of maximum pressure, also linear and disposed longitudinally, retires eastwardly before the advance of the storm and disappears over the Atlantic Ocean as the storm line reaches the western border of New England, after which the line of maximum pressure reappears in the southwest, following up the storm that is now withdrawing beyond the Atlantic coast line. There is little wind near the line of greatest pressure, and in direction it is generally away from the line. Mr. Espy concluded his report by a suggestion which has since then been happily carried into effect: It is highly desirable to surround storms and keep them constantly in view from their beginning to their end. Now, as the barometer generally sinks more during the pas- sage of our great winter storms in the northern part of the United States than in the southern, is it not probable that the northern half of many of these storms is entirely beyond the bounds of our observations? And, as these storms certainly reach New- foundland in their progress toward the east, is it not probable that they do not break up before they advance far into the ocean ? May not some of them even reach the shores of Europe? Under these circumstances would not the governments of England and France, if they were requested by the proper authorities, order the masters of the numerous steamers which now ply the Atlantic to send copies of their journals to Wash- ington City to be collated with those received now from so many other quarters ? What high utilities to the mariner, and through the mariner to all mankind, might not reasonably be anticipated from such a system of wide-spread, simultaneous obser- vations, continued long enough to compare with each other, not merely the storms of different seasons but the storms of different years. The merest glance at Espy's charts demonstrates the fact that tele- graphic communication was the only thing wanting to enable that enthusiast to plan the very weather service that we have at the pres- ent day. Meanwhile, owing to the impetus which he had given to meteorology, a board of officers, consisting of Drs. Mower, Steinecke, and Cuyler, formulated " Directions for taking Meteorological Obser- vations adopted by the Medical Department of the Army," which were published in 1844. Observations were required daily at a little before sunrise, at 9 a. m., and 3 and 9 p. m. on the barometer and its attached thermometer, the detached thermometer, the wind, and the weather; the wet bulb was noted twice only, before sunrise and at 3 p. in. Bunten's siphon barometer, the wet bulb, and a conical rain guage were issued. Tables were given for the conversion of the French barometric scale into English inches, and for the translation of centigrade degrees into those of Fahrenheit's scale. Clearness of sky was directed to be indicated by the numerals 0-10, the first representing no clearness, the last no cloud; the force of wind was to be reported in like manner, 0 signifying a calm and 10 a violent hur- ricane. Hourly observations were called for on the 21st days of March, June, September, and December, beginning at 6 a. m. and ending at the same hour next day. 8 Evidently the Medical Department at this time intended to give renewed energy to the development of meteorological science, for Dr. Mower's paper, already cited and which may be regarded as official, closes with a cordial invitation to colleges, scientific institutions, and individual students of meteorology to co-operate with the department, placing its forms at their disposition and stating that all contribu- tions will be cheerfully acknowledged in the publications of the de- partment. Arrangements, he says, have been made for prosecuting meteorological inquiries with renewed diligence; and a medical officer will shortly be detailed to give his chief time and attention to the subject, to arrange and digest the matter collected, and to pre- pare the results for publication. It was not, however, until 1851 that the next publication from the office of the Surgeon General was issued. " Meteorological Register for twelve years, from 1831 to 1842, inclusive, compiled from observa- tions made by the officers of the Medical Department of the Army at the military posts of the United States, prepared under the direction of Bvt. Brig. Gen. Thomas Lawson, Surgeon General, U. S. Army, Washington, 1851." And notwithstanding the delay in publication no effort was made to collate the observations and deduce general results from the mass of facts presented. The tables embraced the records of 62 posts lying between N. 24° 20', Key West Barracks, and N. 47° 15', Fort Kent, Me., and between W. 66° 58', Fort Sullivan, at Eastport, Me., and W. 95° 10', Fort Gibson, Cherokee Nation, Ark. Five years later appeared a " Statistical Report on the Sickness and Mortality of the Army of the United States, compiled from the Re- ports of the Surgeon General's Office, embracing a period of sixteen years from January, 1839, to January, 1855, prepared, etc., by R. H. Coolidge, Assistant Surgeon, U. S. Army, Washington, 1856." This volume contained a series of tables, one for each of 159 posts, giving the mean results of the observations of temperature for each month, season, and year during the entire period of the observations at each. The rainfall, wind, and weather were given in another series of tables. A similar statistical report was issued in 1860, covering the period of five years, January, 1855, to January, 1860, also by Dr. Coolidge. This brings us to the war of the rebellion, with the meteorological records of forty years before the public. The original reports had often been consulted by officers engaged in explorations for a railroad from the Mississippi to the Pacific and on various boundary surveys, and by those desirous of elucidating some special point in meteor- ology. From January, 1819, to January, 1841, the observations were made three times daily, at 7 a. m., 2 and 9 p. m.; in 1841 at sunrise, 2 and 9 p. m.; in 1842 at sunrise, 2 p. m., sunset, and 9 p. m.; in 1843-'55 at a little before sunrise, 9 a. m., and 2 and 9 p. m.; but as an extended examination of the records of the hourly observations 9 showed that the mean of the observations taken at 7 a. m., and 2 and 9 p. m. more nearly approximated the true daily mean than did the means of any of the four daily observations, orders were issued direct- ing a return to the three daily observations at those hours. In following up the connection of the Medical Department of the Army with the progress of meteorological science, it is proper at this stage to refer to the history of one member of the Department, Assist- ant Surg. A. J. Myer. This officer was appointed in 1854 and served until 1860, when he vacated his position to accept that of Signal Officer of the Army. During his frontier service he drafted a code of signals which, in 1858, was approved by a board of critical officers. With his efforts to build up a valuable signal service and the difficulties he encountered this paper has no concern, nor with his ultimate suc- cess in obtaining legislation for a signal corps organization at a time when, through the antagonism of the Secretary of War, he was relieved from its command. During the war of the rebellion the discovery and transmission of information regarding the movements of the enemy's forces and the well-being of our own absorbed all the energies of the newly-formed corps, but at its close in 1866, when the military establishment was reduced to a peace footing, Gen. Myer, who had happily been recalled to the head of the Signal Corps, looked natu- rally for some service or duty for his command in line with its military duties that would enable it to be of value to the country during the coming years of peace. Nonmilitary work by military men was no innovation in this country, for the Engineer Department of the Army had in times of peace surveyed the Western Territories, built bridges and levees, deepened rivers and harbors, and constructed many important works of internal improvement. Gen. Myer's six years of service as a post surgeon, during which he became familiar with the meteorological work of the Medical Department and the progress of storms across the continent as developed by Mr. Espy, led him to urge upon Congress the advantageous possibilities sug- gested by the observation of storms and the prompt signalling of their approach. Not until February, 1870, however, was he author- ized to undertake this work, when he immediately established 66 sta- tions, equipping each observer as he himself had formerly been equipped by the Medical Department, but furnishing in addition an anemometer to obtain a more precise knowledge of the force of coming storms. Each observer transmitted his observations by telegraph to the central station at Headquarters of the Signal Corps, Washington, D. C., where all were plotted on a skeleton map and studied to de- termine the atmospheric conditions and the movements and forces of storms in precisely the same way that Mr. Espy dealt with the data which he received by mail long after the occurrence of the events. Mr. Espy knew how the storm had traveled; Gen. Myer knew how 1 2 10 the storm was traveling. This constituted the difference between the old and the new. The former published his knowledge of the completed event as a contribution to science and the possibilities of the future; the latter conveyed his knowledge of the coming event by telegraph and signals to all who were concerned in the progress of the passing storm. Subsequently, Gen. Myer established an Inter- national Weather Bulletin and Weather Map based on simultaneous observations, thus carrying into present practice the suggestion con- tained in that paragraph of Mr. Espy's report that has just been cited. Since 1874 all meteorological reports from Army Medical Officers have been turned over to the Chief Signal Officer or to his successor in charge of the Weather Bureau. It might be supposed that since the value of this Bureau has been so thoroughly established its im- portant position would render it wholly independent of the officers whose labors in the past had done so much to establish it; but this is not so. Meteorological observations have been discontinued at those military posts near which the Weather Bureau has installed its observers, but there are yet many parts of our vast country occupied by military posts where no station of the Weather Service has been established. At these military posts, some 50 in number, medical officers continue to make their meteorological observations as their predecessors did in the early days after the issuance of the order of May 2, 1814, which made it the duty of hospital surgeons to keep a diary of the weather. Long and faithfully have the medical officers of the Army obeyed that order, and with honorable pride they can point to the results that have been achieved.