Latitudinal distribution of freon 11 and methylchloroform in the Pacific atmosphere
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OLR(1982)29(12) 761 the oceans if a 1.56 /Lm (instead of a 0.75 /~m) waveband is used. NASA Langley Res. Center, Hampton, Va. 23665, USA. B350. Pollution 82:5983 Kazakov, Iu.E., V.M. Koropalov and I.M. Nazarov, 1982. Latitudinal distribution of freon 11 and methylchloroform in the Pacific atmosphere. Dokl. Akad. Nauk SSSR, 263(5):1095-1098. (In Russian.) 82:5984 M6sz,~tros, E., 1982. On the atmospheric input of sulfur into the ocean. Tellus, 34(3):277-282. The dry deposition of S onto the ocean surface is calculated using results of trace gas and aerosol measurements in the marine boundary layer and information on the deposition velocity of different materials at the air-sea interface. Precipitation input is estimated based on composition at Hawaii, American Samoa and the west coast of Ireland. Total air-sea transfer of S equals 324 Tg yr ~, the major part (82%) carried down by precipitation. Excess sulfate in the marine atmosphere accounts for 50% of the total input. Inst. for Atmospheric Phys., P.O.B. 39, H-1675 Budapest, Hungary. 82:5985 Wisniewski, Joe, 1982. The potential acidity asso- ciated with dews, frosts, and fogs. Wat. Air Soil Pollut., 17(4):361-377. Flow General Inc., 7655 Old Springhouse Rd., McLean, Va. 22102, USA. B380. Forecasting 82:5986 De Las Alas, J.G., 1981. The application of the barotropic model in typhoon track prediction. Nat. appl. Sci. Bull., 33(1/2):75-83. Dept. of Meteorol. and Oceanogr., Univ. of Philippines, Manila, Philippines. 82:5987 Tice, T.F. et al., 1981/82. Economic and social value of weather and climate information, (Symposium, January 1981, San Diego.) Special section. J. appl. Met., 21(4):447-539; 12 papers. The bulk of symposium papers considered the agricultural value of weather forecasting. Some less well-known applications of such information were discussed including natural disaster insurance rate- setting, managing energy resources, and deciding whether to 'wrap or not' newspapers scheduled for home delivery. (isz) B450. Miscellaneous 82:5988 Levine, J.S. and Frank Allario, 1982. The global troposphere: biogeochemical cycles, chemistry, and remote sensing. Environ. Monit. Assessment, 1(3):263-306. Biogeochemical cycles and atmospheric chemistry which control and modulate the natural troposphere are reviewed in this 43-page paper; the impact of anthropogenic activities on these cycles is consid- ered. Current measurement needs, present and future remote sensing capabilities, instrumentation, and technology are discussed; improvements in remote sensing technology are proposed. NASA Langley Res. Center, Hampton, Va. 23665, USA. (jch) C. CHEMICAL OCEANOGRAPHY C10. Apparatus and methods 82:5989 Dandonneau, Yves, 1982. A method for the rapid determination of chlorophyll plus plmeopigments in samples collected by merchant ships. Deep-Sea Res., 29(5A):647-654. Samples are filtered through Millipore ® HA filters which are stored dry and in the dark for later analysis. Measurement is without extraction; filters are arranged on a thin-layer chromatography glass plate and processed by a fluorometer fitted with a TLC scanning door. A 20-day delay is necessary before the measurements; after 20 days, the fluo-
Transcript of Latitudinal distribution of freon 11 and methylchloroform in the Pacific atmosphere
OLR(1982)29(12) 761
the oceans if a 1.56 /Lm (instead of a 0.75 /~m) waveband is used. NASA Langley Res. Center, Hampton, Va. 23665, USA.
B350. Pollution
82:5983 Kazakov, Iu.E., V.M. Koropalov and I.M. Nazarov,
1982. Latitudinal distribution of freon 11 and methylchloroform in the Pacific atmosphere. Dokl. Akad. Nauk SSSR, 263(5):1095-1098. (In Russian.)
82:5984 M6sz,~tros, E., 1982. On the atmospheric input of
sulfur into the ocean. Tellus, 34(3):277-282.
The dry deposition of S onto the ocean surface is calculated using results of trace gas and aerosol measurements in the marine boundary layer and information on the deposition velocity of different materials at the air-sea interface. Precipitation input is estimated based on composition at Hawaii, American Samoa and the west coast of Ireland. Total air-sea transfer of S equals 324 Tg y r ~, the major part (82%) carried down by precipitation. Excess sulfate in the marine atmosphere accounts for 50% of the total input. Inst. for Atmospheric Phys., P.O.B. 39, H-1675 Budapest, Hungary.
82:5985 Wisniewski, Joe, 1982. The potential acidity asso-
ciated with dews, frosts, and fogs. Wat. Air Soil Pollut., 17(4):361-377. Flow General Inc., 7655 Old Springhouse Rd., McLean, Va. 22102, USA.
B380. Forecasting
82:5986 De Las Alas, J.G., 1981. The application of the
barotropic model in typhoon track prediction. Nat. appl. Sci. Bull., 33(1/2):75-83. Dept. of Meteorol. and Oceanogr., Univ. of Philippines, Manila, Philippines.
82:5987 Tice, T.F. et al., 1981/82. Economic and social value
of weather and climate information, (Symposium, January 1981, San Diego.) Special section. J. appl. Met., 21(4):447-539; 12 papers.
The bulk of symposium papers considered the agricultural value of weather forecasting. Some less well-known applications of such information were discussed including natural disaster insurance rate- setting, managing energy resources, and deciding whether to 'wrap or not' newspapers scheduled for home delivery. (isz)
B450. Miscellaneous
82:5988 Levine, J.S. and Frank Allario, 1982. The global
troposphere: biogeochemical cycles, chemistry, and remote sensing. Environ. Monit. Assessment, 1(3):263-306.
Biogeochemical cycles and atmospheric chemistry which control and modulate the natural troposphere are reviewed in this 43-page paper; the impact of anthropogenic activities on these cycles is consid- ered. Current measurement needs, present and future remote sensing capabilities, instrumentation, and technology are discussed; improvements in remote sensing technology are proposed. NASA Langley Res. Center, Hampton, Va. 23665, USA. (jch)
C. CHEMICAL OCEANOGRAPHY
C10. Apparatus and methods
82:5989 Dandonneau, Yves, 1982. A method for the rapid
determination of chlorophyll plus plmeopigments in samples collected by merchant ships. Deep-Sea Res., 29(5A):647-654.
Samples are filtered through Millipore ® HA filters which are stored dry and in the dark for later analysis. Measurement is without extraction; filters are arranged on a thin-layer chromatography glass plate and processed by a fluorometer fitted with a TLC scanning door. A 20-day delay is necessary before the measurements; after 20 days, the fluo-
