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Books on the topic 'Tropospheric aerosols'

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1

Fortmann, Martin. Zum Einfluss troposphärischer Aerosole auf das Klima der Arktis =: Influence of tropospheric aerosols on the Arctic climate. Bremerhaven: Alfred-Wegener-Institut für Polar- und Meeresforschung, 2004.

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2

Schumacher, Rolf. Messung von optischen Eigenschaften troposphärischer Aerosols in der Arktis =: Measurements of optical properties for tropospheric aerosols in the Arctic. Bremerhaven: Alfred-Wegener-Institut für Polar- und Meeresforschung, 2001.

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3

Piel, Claudia. Variabilität chemischer und physikalischer Parameter des Aerosols in der antarktischen Troposphäre =: Variability of chemical and physical parameters of aerosol in the Antarctic troposphere. Bremerhaven: Alfred-Wegener-Institut für Polar- und Meeresforschung, 2004.

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4

Mieding, Birgit. Rekonstruktion tausendjähriger aerosolchemischer Eiskernzeitreihen aus Nordostgrönland: Quantifizierung zeitlicher Veränderungen in Atmosphärenzirkulation, Emission und Deposition = Reconstruction of millenial aerosol-chemical ice core records from the northeast Greenland : quantification of termporal changes in atmospheric circulation, emission and deposition. Bremerhaven: Alfred-Wegener-Institut für Polar- und Meeresforschung, 2005.

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5

Experts Meeting on Space Observations of Tropospheric Aerosols and Complementary Measurements (1989 Hampton, Va.). Report of the Experts Meeting on Space Observations of Tropospheric Aerosols and Complementary Measurements, Hampton, Virginia, 15-18 November 1989 (IACP-2). [Paris]: International Council of Scientific Unions ; [Geneva], 1990.

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6

Schmidt, Anja. Modelling Tropospheric Volcanic Aerosol. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-34839-6.

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7

Reinhold, Reiter. Fields, Currents and aerosols in the lower troposphere. Rotterdam: A.A. Balkeme, 1986.

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8

Reinhold, Reiter. Fields, currents and aerosols in the lower troposphere. New Delhi: Amerind Pub., 1985.

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9

WMO Technical Conference on the Monitoring and Assessment of Changing Composition of the Troposphere (1989 Sofia, Bulgaria). Changing composition of the troposphere: Extended abstracts of papers presented at the WMO Technical Conference on the Monitoring and Assessment of Changing Composition of the Troposphere : Sofia, 23-27 October 1989. Geneva, Switzerland: Secretariat of the World Meteorological Organization, 1989.

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10

International, Laser Radar Conference (19th 1998 Annapolis Md ). Nineteenth International Laser Radar Conference: Abstracts of papers presented at a conference sponsored by the National Aeronautics and Space Administration, Washington, D.C. ... [et al.], and held at the United States Naval Academy, Annapolis, Maryland, July 6-10, 1998. Hampton, Va: National Aeronautics and Space Administration, Langley Research Center, 1998.

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11

Peter, Warneck, ed. Heterogeneous and liquid phase processes: Laboratory studies related to aerosols and clouds. Berlin: Springer, 1996.

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12

Warneck, Peter. Heterogeneous and Liquid Phase Processes: Laboratory Studies Related to Aerosols and Clouds (Transport and Chemical Transformation of Pollutants in t. Springer Verlag, 1996.

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13

Warneck, Peter. Heterogeneous and Liquid Phase Processes: Laboratory Studies Related to Aerosols and Clouds (Transport and Chemical Transformation of Pollutants in the Troposphere, V. 2). Springer, 1996.

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14

Chʻen, Hsiao-chʻing. Oxygenated natural products in tropospheric aerosols-sources and transport. 1991.

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15

Standley, Laurel J. Determination of molecular signatures of natural and thermogenic products in tropospheric aerosols--input and transport. 1987.

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16

S, Levine Joel, Langley Research Center, United States. Office of Space Science and Applications, and United States. National Aeronautics and Space Administration. Scientific and Technical Information Branch, eds. Space opportunities for tropospheric chemistry research: Proceedings of a workshop. [Washington, D.C.]: National Aeronautics and Space Administration, Scientific and Technical Information Branch, 1987.

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17

Space opportunities for tropospheric chemistry research: Proceedings of a workshop sponsored by the NASA Office of Space Science and Applications, Washington, D.C., and NASA Langley Research Center, Hampton, Virginia, and held in New York City, New York, September 9-13, 1985. Washington, D.C: National Aeronautics and Space Administration, Scientific and Technical Information Branch, 1987.

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18

1936-, Hobbs Peter Victor, McCormick M. Patrick, International Association of Meteorology and Atmospheric Physics., International Union of Geodesy and Geophysics. General Assembly, and Symposium on Aerosols and Climate (1987 : University of British Columbia), eds. Aerosols and climate. Hampton, Va., USA: A. Deepak Pub., 1988.

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19

Braban, Christine Fiona. Laboratory studies of model tropospheric aerosol phase transitions. 2004.

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20

Schmidt, Anja. Modelling Tropospheric Volcanic Aerosol: From Aerosol Microphysical Processes to Earth System Impacts. Springer, 2015.

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21

Schmidt, Anja. Modelling Tropospheric Volcanic Aerosol: From Aerosol Microphysical Processes to Earth System Impacts. Springer, 2013.

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22

Reiter, R. Fields, Currents, and Aerosols in the Lower Troposphere. South Asia Books, 1987.

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23

R, Cutten D., and United States. National Aeronautics and Space Administration., eds. Multiwavelength comparison of modeled and measured remote tropospheric aerosol backscatter over Pacific Ocean. [Washington, DC: National Aeronautics and Space Administration, 1996.

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24

Goswami, B. N., and Soumi Chakravorty. Dynamics of the Indian Summer Monsoon Climate. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.613.

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Abstract:
Lifeline for about one-sixth of the world’s population in the subcontinent, the Indian summer monsoon (ISM) is an integral part of the annual cycle of the winds (reversal of winds with seasons), coupled with a strong annual cycle of precipitation (wet summer and dry winter). For over a century, high socioeconomic impacts of ISM rainfall (ISMR) in the region have driven scientists to attempt to predict the year-to-year variations of ISM rainfall. A remarkably stable phenomenon, making its appearance every year without fail, the ISM climate exhibits a rather small year-to-year variation (the standard deviation of the seasonal mean being 10% of the long-term mean), but it has proven to be an extremely challenging system to predict. Even the most skillful, sophisticated models are barely useful with skill significantly below the potential limit on predictability. Understanding what drives the mean ISM climate and its variability on different timescales is, therefore, critical to advancing skills in predicting the monsoon. A conceptual ISM model helps explain what maintains not only the mean ISM but also its variability on interannual and longer timescales.The annual ISM precipitation cycle can be described as a manifestation of the seasonal migration of the intertropical convergence zone (ITCZ) or the zonally oriented cloud (rain) band characterized by a sudden “onset.” The other important feature of ISM is the deep overturning meridional (regional Hadley circulation) that is associated with it, driven primarily by the latent heat release associated with the ISM (ITCZ) precipitation. The dynamics of the monsoon climate, therefore, is an extension of the dynamics of the ITCZ. The classical land–sea surface temperature gradient model of ISM may explain the seasonal reversal of the surface winds, but it fails to explain the onset and the deep vertical structure of the ISM circulation. While the surface temperature over land cools after the onset, reversing the north–south surface temperature gradient and making it inadequate to sustain the monsoon after onset, it is the tropospheric temperature gradient that becomes positive at the time of onset and remains strongly positive thereafter, maintaining the monsoon. The change in sign of the tropospheric temperature (TT) gradient is dynamically responsible for a symmetric instability, leading to the onset and subsequent northward progression of the ITCZ. The unified ISM model in terms of the TT gradient provides a platform to understand the drivers of ISM variability by identifying processes that affect TT in the north and the south and influence the gradient.The predictability of the seasonal mean ISM is limited by interactions of the annual cycle and higher frequency monsoon variability within the season. The monsoon intraseasonal oscillation (MISO) has a seminal role in influencing the seasonal mean and its interannual variability. While ISM climate on long timescales (e.g., multimillennium) largely follows the solar forcing, on shorter timescales the ISM variability is governed by the internal dynamics arising from ocean–atmosphere–land interactions, regional as well as remote, together with teleconnections with other climate modes. Also important is the role of anthropogenic forcing, such as the greenhouse gases and aerosols versus the natural multidecadal variability in the context of the recent six-decade long decreasing trend of ISM rainfall.
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25

Tropospheric Aerosol Formation Transformation Fate And Impacts University Of Leeds United Kingdom 2224 July 2013. Royal Society of Chemistry, 2014.

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26

V, Browell Edward, and United States. National Aeronautics and Space Administration., eds. Airborne lidar measurements of aerosols, mixed layer heights, and ozone during the 1980 PEPE/NEROS summer field experiment. Washington, D.C: National Aeronautics and Space Administration, Scientific and Technical Information Branch, 1985.

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27

Dieter, Ehhalt, Pearman G. I, Galbally I. E, Commonwealth Scientific and Industrial Research Organization (Australia), Australia Bureau of Meteorology, and Conference on the Scientific Application of Baseline Observations of Atmospheric Composition (1984 : CSIRO Division of Atmospheric Research), eds. Scientific application of baseline observations of atmospheric composition (SABOAC). Dordrecht: D. Reidel Pub. Co., 1987.

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28

Changing composition of the troposphere: Extended abstracts of papers presented at the WMO Technical Conference on the Monitoring and Assessment of Changing ... October 1989 (Special environmental report). Secretariat of the World Meteorological Organization, 1989.

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29

United States. National Aeronautics and Space Administration., ed. Effects of subsonic aircraft on aerosols and cloudiness in the upper troposphere and lower stratosphere: Summary of research, period: 1 September 1994 - 1 September 1997, grant no.: NAG5-2711. [Washington, DC: National Aeronautics and Space Administration, 1997.

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30

United States. National Aeronautics and Space Administration., ed. Effects of subsonic aircraft on aerosols and cloudiness in the upper troposphere and lower stratosphere: Summary of research, period: 1 September 1994 - 1 September 1997, grant no.: NAG5-2711. [Washington, DC: National Aeronautics and Space Administration, 1997.

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31

United States. National Aeronautics and Space Administration., ed. Effects of subsonic aircraft on aerosols and cloudiness in the upper troposphere and lower stratosphere: Summary of research, period: 1 September 1994 - 1 September 1997, grant no.: NAG5-2711. [Washington, DC: National Aeronautics and Space Administration, 1997.

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32

(Editor), Sandro Fuzzi, and Dietmar Wagenbach (Editor), eds. Cloud Multi-phase Processes and High Alpine Air and Snow Chemistry: Ground-based Cloud Experiments and Pollutant Deposition in the High Alps (Transport ... of Pollutants in the Troposphere). Springer, 1997.

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33

Pierre-Yves, Deschamps, and United States. National Aeronautics and Space Administration., eds. Inversion schemes to retrieve atmospheric and oceanic parameters from SeaWiFS data. [Washington, DC: National Aeronautics and Space Administration, 1997.

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34

N, Singh Upendra, Ismail Syed, Schwemmer Geary K, Langley Research Center, and United States. National Aeronautics and Space Administration., eds. Nineteenth International Laser Radar Conference. Hampton, Va: National Aeronautics and Space Administration, Langley Research Center, 1998.

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