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Books on the topic 'Stratosphere dynamics'

Author: Grafiati
Published: 4 June 2021
Last updated: 9 February 2022

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1

Polvani, L. M., A. H. Sobel, and D. W. Waugh, eds. The Stratosphere: Dynamics, Transport, and Chemistry. Washington, D. C.: American Geophysical Union, 2010. http://dx.doi.org/10.1029/gm190.

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2

The stratosphere: Dynamics, transport, and chemistry. Washington, DC: American Geophysical Union, 2010.

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3

Müller, Marion. Polare Stratosphärenwolken und mesoskalige Dynamik am Polarwirbelrand = Polar stratospheric clouds and mesoscale dynamics at the Polar vortex edge. Bremerhaven: Alfred-Wegener-Institut für Polar- und Meeresforschung, 2001.

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4

Bowman, Kenneth P. Studies of dynamical processes affecting the distribution of stratospheric ozone: Final report. [Washington, DC: National Aeronautics and Space Administration, 1993.

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5

Miles, Thomas. Comparison of satellite-derived dynamical quantities for the stratosphere of the Southern Hemisphere: Proceedings of a workshop sponsored by the National Aeronautics and Space Administration, Washington, D.C, and held in Williamsburg, Virginia, April 14-17, 1986. Hampton , Va: Langley Research Center, 1989.

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6

Heese, Birgit. Untersuchungen zum Beitrag chemischer und dynamischer Prozesse zur Variabilität des stratosphärischen Ozons über der Arktis =: Investigations of contributions by chemical and dynamical processes to the variability of stratospheric ozone above the Arctic. Bremerhaven: Alfred-Wegener-Institut für Polar- und Meeresforschung, 1996.

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7

Polvani, L. M., A. H. Sobel, and D. W. Waugh. Stratosphere: Dynamics, Transport, and Chemistry. American Geophysical Union, 2013.

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8

Polvani, L. M., A. H. Sobel, and D. W. Waugh. Stratosphere: Dynamics, Transport, and Chemistry. American Geophysical Union, 2013.

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9

Polvani, L. M., A. H. Sobel, and D. W. Waugh. Stratosphere: Dynamics, Transport, and Chemistry. American Geophysical Union, 2013.

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10

United States. National Aeronautics and Space Administration., ed. Large-scale dynamics and transport in the stratosphere. [Washington, D.C: National Aeronautics and Space Administration, 1990.

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11

United States. National Aeronautics and Space Administration., ed. Large-scale dynamics and transport in the stratosphere. [Washington, D.C: National Aeronautics and Space Administration, 1990.

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12

United States. National Aeronautics and Space Administration., ed. Wave dynamics and transport in the stratosphere: Final technical report. [Washington, DC: National Aeronautics and Space Administration, 1985.

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13

Behera, Swadhin, and Toshio Yamagata. Climate Dynamics of ENSO Modoki Phenomena. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.612.

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The El Niño Modoki/La Niña Modoki (ENSO Modoki) is a newly acknowledged face of ocean-atmosphere coupled variability in the tropical Pacific Ocean. The oceanic and atmospheric conditions associated with the El Niño Modoki are different from that of canonical El Niño, which is extensively studied for its dynamics and worldwide impacts. A typical El Niño event is marked by a warm anomaly of sea surface temperature (SST) in the equatorial eastern Pacific. Because of the associated changes in the surface winds and the weakening of coastal upwelling, the coasts of South America suffer from widespread fish mortality during the event. Quite opposite of this characteristic change in the ocean condition, cold SST anomalies prevail in the eastern equatorial Pacific during the El Niño Modoki events, but with the warm anomalies intensified in the central Pacific. The boreal winter condition of 2004 is a typical example of such an event, when a tripole pattern is noticed in the SST anomalies; warm central Pacific flanked by cold eastern and western regions. The SST anomalies are coupled to a double cell in anomalous Walker circulation with rising motion in the central parts and sinking motion on both sides of the basin. This is again a different feature compared to the well-known single-cell anomalous Walker circulation during El Niños. La Niña Modoki is the opposite phase of the El Niño Modoki, when a cold central Pacific is flanked by warm anomalies on both sides.The Modoki events are seen to peak in both boreal summer and winter and hence are not seasonally phase-locked to a single seasonal cycle like El Niño/La Niña events. Because of this distinction in the seasonality, the teleconnection arising from these events will vary between the seasons as teleconnection path will vary depending on the prevailing seasonal mean conditions in the atmosphere. Moreover, the Modoki El Niño/La Niña impacts over regions such as the western coast of the United States, the Far East including Japan, Australia, and southern Africa, etc., are opposite to those of the canonical El Niño/La Niña. For example, the western coasts of the United States suffer from severe droughts during El Niño Modoki, whereas those regions are quite wet during El Niño. The influences of Modoki events are also seen in tropical cyclogenesis, stratosphere warming of the Southern Hemisphere, ocean primary productivity, river discharges, sea level variations, etc. A remarkable feature associated with Modoki events is the decadal flattening of the equatorial thermocline and weakening of zonal thermal gradient. The associated ocean-atmosphere conditions have caused frequent and persistent developments of Modoki events in recent decades.
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14

T, Miles, O'Neill Alan 1950-, and United States. National Aeronautics and Space Administration., eds. Comparison of satellite-derived dynamical quantities for the stratosphere of the Southern Hemisphere: Proceedings of a workshop. Washington, D.C: National Aeronautics and Space Administration, Office of Management, Scientific and Technical Information Division, 1989.

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15

Lippmann, Morton, and Richard B. Schlesinger. Dispersion of Contaminants. Oxford University Press, 2017. http://dx.doi.org/10.1093/med/9780190688622.003.0004.

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This chapter describes the pathways and dynamics of chemical contaminants within the various structural layers. In the atmosphere, the chemical contaminants are transferred by diffusion, turbulence, plume dispersion, long-range transport, and tropospheric-stratospheric interchange. They are transferred to the hydrosphere by surface deposition, rainout, and washout. They are transferred to the lithosphere by surface flow and penetration, and are transferred within the biosphere by food-chain concentration.
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16

United States. National Aeronautics and Space Administration., ed. The effect of enhanced diabatic heating on stratospheric circulation: A dissertation ... [Washington, D.C: National Aeronautics and Space Administration, 1997.

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17

I, Ivanovskiĭ A., and Gosudarstvennyĭ komitet SSSR po gidrometeorologii i kontroli͡u︡ prirodnoĭ sredy., eds. Fizika verkhneĭ atmosfery. Moskva: Moskovskoe otd-nie Gidrometeoizdata, 1985.

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18

J, Gierasch Peter, Leroy Stephen S, and United States. National Aeronautics and Space Administration., eds. Temperature and circulation in the stratospheres of the outer planets. [Washington, DC: National Aeronautics and Space Administration, 1989.

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19

Wenjie, Hu, Ko Malcolm K. W, and United States. National Aeronautics and Space Administration., eds. Quarterly progress report on the utilization of UARS data in validation of photochemical and dynamical mechanism in stratospheric models: (contract NAS5-32844). [Cambridge, Mass: Atmospheric and Environmental Research, Inc.], 1995.

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20

Utilization of UARS data in validation of photochemical and dynamical mechanisms in stratospheric models: Contract NAS5-32844. [Washington, DC: National Aeronautics and Space Administration, 1998.

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21

Wenjie, Hu, Ko Malcolm K. W, and United States. National Aeronautics and Space Administration., eds. Quarterly progress report on the utilization of UARS data in validation of photochemical and dynamical mechanism in stratospheric models: (contract NAS5-32844). [Washington, DC: National Aeronautics and Space Administration, 1996.

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22

Wenjie, Hu, Ko Malcolm K. W, and United States. National Aeronautics and Space Administration., eds. Quarterly progress report on the utilization of UARS data in validation of photochemical and dynamical mechanism in stratospheric models: (contract NAS5-32844). [Cambridge, Mass: Atmospheric and Environmental Research, Inc.], 1995.

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23

Wenjie, Hu, Ko Malcolm K. W, and United States. National Aeronautics and Space Administration., eds. Quarterly progress report on the utilization of UARS data in validation of photochemical and dynamical mechanism in stratospheric models: (contract NAS5-32844). [Cambridge, Mass: Atmospheric and Environmental Research, Inc., 1995.

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24

Wenjie, Hu, Ko Malcolm K. W, and United States. National Aeronautics and Space Administration., eds. Quarterly progress report on the utilization of UARS data in validation of photochemical and dynamical mechanism in stratospheric models: (contract NAS5-32844). [Washington, DC: National Aeronautics and Space Administration, 1996.

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25

Wenjie, Hu, Ko Malcolm K. W, and United States. National Aeronautics and Space Administration., eds. Quarterly progress report on the utilization of UARS data in validation of photochemical and dynamical mechanism in stratospheric models: (contract NAS5-32844). [Cambridge, Mass: Atmospheric and Environmental Research, Inc., 1995.

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26

[Study of atmospheric dynamics]: Final report of work completed under NAS8-36718 for the period, September 4th, 1986 - July 31st, 1993. [Washington, DC: National Aeronautics and Space Administration, 1993.

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27

Center, Ames Research, ed. Computation of the fluid and optical fields about the stratospheric observatory for infrared astronomy (SOFIA) and the coupling of fluids, dynamics, and control laws on parallel computers. San Jose, CA: MCAT Institute, 1993.

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