Report of the Inter-American Tropical Tuna Commission for the year 1957

ENGLISH: The Inter-American Tropical Tuna Commission was established under authority of a Convention between the Governments of Costa Rica and the United States, which entered into force in 1950_ The Convention provides for the adherence of other governments having an interest in the tuna and tuna-bait resources of the Eastern Tropical Pacific Ocean, by exchange of correspondence with existing members. Panama adhered to the Convention in 1953. SPANISH: La Comisión Interamericana del Atún Tropical fué establecida en virtud de una Convención entre los Gobiernos de Costa Rica y de los Estados Unidos, cuya vigencia comenzó en 1950. Dicha Convención permite la entrada de otros gobiernos que tengan interés en los recursos de atún y de peces de carnada para su pesca en el Océano Pacífico Oriental Tropical, mediante el intercambio de correspondencia con los países firmantes. Panamá se adhirió a la Convención en 1953. (PDF contains 134 pages.)

Report of the Inter-American Tropical Tuna Commission for the year 1958

ENGLISH: The Inter-American Tropical Tuna Commission was established by a Convention, between the Governments of Costa Rica and the United States, which entered into force in 1950. Under a provision of the Convention inviting the adherence of other nations having an interest in the tuna and tuna-bait resources of the Eastern Tropical Pacific Ocean, Panama also adhered in 1953. SPANISH: La Comisión Interamericana del Atún Tropical fué establecida por una Convención entre los Gobiernos de Costa Rica y de los Estados Unidos, la cual entró en vigencia en 1950. Panamá se adhirió a la Convención en 1953, de conformidad con una cláusula que deja la puerta abierta a los otros paises interesados en los recursos atuneros y de carnada para el atún del Océano Pacifico Oriental Tropical. (PDF contains 121 pages.)

Report of the Inter-American Tropical Tuna Commission for the year 1959

ENGLISH: The Inter-American Tropical Tuna Commission was established under authority of a Convention, between the Governments of the Republic of Costa Rica and the United States of America, which entered into force in 1950. The Convention provides for the adherence, by exchange of correspondence with existing members, of other governments having an interest in the tuna and tuna-bait resources of the Eastern Tropical Pacific Ocean. The Republic of Panama adhered to the Convention in 1953. SPANISH: La Comisión Interamericana del Atún Tropical fue establecida en virtud de una Convención suscrita entre los Gobiernos de la Republica de Costa Rica y de los Estados Unidos de America, que entro en vigencia en 1950. La Convención esta abierta para que otros gobiernos interesados en los recursos de atún y de carnada para la pesca de este en el Océano Pacifico Oriental Tropical puedan adherirse a la misma mediante intercambio de correspondencia con los Gobiernos Miembros. La Republica de Panamá se adhirió a la Convención en 1953. (PDF contains 156 pages.)

Report of the Inter-American Tropical Tuna Commission for the year 1960

ENGLISH: The Inter-American Tropical Tuna Commission operates under the authority of a Convention, originally negotiated between the Governments of the Republic of Costa Rica and the United States of America, which entered into force in 1950. The Republic of Panama adhered to the Convention in 1953. The Convention is open to adherence of other nations having an interest in the tuna and tuna-bait resources of the Eastern Tropical Pacific Ocean. SPANISH: La Comisión Interamericana del Atún Tropical funciona bajo la autoridad de una Convención que originalmente fue negociada entre los Gobiernos de la Republica de Costa Rica y de los Estados Unidos de America y entro en vigencia en 1950; la Republica de Panamá se adhirió a la Convención en 1953. Esta Convención esta abierta para otras naciones que tengan interés en los recursos de atún y de las especies de carnada en el Océano Pacifico Oriental Tropical (PDF contains 183 pages.)

1976 step in the Pacific climate: forty environmental changes between 1968-1975 and 1977-1984

Examination of 40 time series of multidisciplinary environmental variables from the Pacific Ocean and the Americas, collected in 1968 to 1984, demonstrated the remarkable consistency of a major climate-related, step-like change in 1976. To combine the 40 variables (e.g., air and water temperatures, Southern Oscillation, chlorophyll, geese, salmon, crabs, glaciers, atmospheric dust, coral, carbon dioxide, winds, ice cover, Bering Strait transport) into a single time series, standard variants of individual annual values (subtracting the mean and dividing by a standard deviation) were averaged. Analysis of the resulting time series showed that the single step in 1976, separating the 1968-1975 period from the 1977-1984 period, accounted for 89% of variance within the composite time series. Apparently, one of the Earth's large ecosystems occasionally undergoes large abrupt shifts.

I. Foehn winds of southern California. II. Foehn wind cyclo-genesis. III. Weather conditions associated with the Akron disaster. IV. The Los Angeles storm of December 30, 1933 to January 1, 1934

I. Foehn winds of southern California.
An investigation of the hot, dry and dust laden winds occurring in the late fall and early winter in the Los Angeles Basin and attributed in the past to the influences of the desert regions to the north revealed that these currents were of a foehn nature. Their properties were found to be entirely due to dynamical heating produced in the descent from the high level areas in the interior to the lower Los Angeles Basin. Any dust associated with the phenomenon was found to be acquired from the Los Angeles area rather than transported from the desert. It was found that the frequency of occurrence of a mild type foehn of this nature during this season was sufficient to warrant its classification as a winter monsoon. This results from the topography of the Los Angeles region which allows an easy entrance to the air from the interior by virtue of the low level mountain passes north of the area. This monsoon provides the mild winter climate of southern California since temperatures associated with the foehn currents are far higher than those experienced when maritime air from the adjacent Pacific Ocean occupies the region.

II. Foehn wind cyclo-genesis.
Intense anticyclones frequently build up over the high level regions of the Great Basin and Columbia Plateau which lie between the Sierra Nevada and Cascade Mountains to the west and the Rocky Mountains to the east. The outflow from these anticyclones produce extensive foehns east of the Rockies in the comparatively low level areas of the middle west and the Canadian provinces of Alberta and Saskatchewan. Normally at this season of the year very cold polar continental air masses are present over this territory and with the occurrence of these foehns marked discontinuity surfaces arise between the warm foehn current, which is obliged to slide over a colder mass, and the Pc air to the east. Cyclones are easily produced from this phenomenon and take the form of unstable waves which propagate along the discontinuity surface between the two dissimilar masses. A continual series of such cyclones was found to occur as long as the Great Basin anticyclone is maintained with undiminished intensity.

III. Weather conditions associated with the Akron disaster.
This situation illustrates the speedy development and propagation of young disturbances in the eastern United States during the spring of the year under the influence of the conditionally unstable tropical maritime air masses which characterise the region. It also furnishes an excellent example of the superiority of air mass and frontal methods of weather prediction for aircraft operation over the older methods based upon pressure distribution.

IV. The Los Angeles storm of December 30, 1933 to January 1, 1934.
This discussion points out some of the fundamental interactions occurring between air masses of the North Pacific Ocean in connection with Pacific Coast storms and the value of topographic and aerological considerations in predicting them. Estimates of rainfall intensity and duration from analyses of this type may be made and would prove very valuable in the Los Angeles area in connection with flood control problems.