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Books on the topic 'Intraseasonal Oscillation in Atmosphere'

Author: Grafiati

Published: 6 September 2023

Last updated: 31 July 2025

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1

Lau, William K. M., and Duane E. Waliser. Intraseasonal Variability in the Atmosphere-Ocean Climate System. Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-13914-7.

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Lau, William K. M. Intraseasonal Variability in the Atmosphere-Ocean Climate System. Springer Berlin Heidelberg, 2012.

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3

E, Waliser Duane, ed. Intraseasonal variability in the atmosphere-ocean climate system. Springer-Verlag, 2005.

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4

G, Vincent Dayton, and United States. National Aeronautics and Space Administration., eds. Relationship between intraseasonal oscillation and subtropical wind maxima over the South Pacific Ocean. National Aeronautics and Space Administration, 1991.

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5

Allan, Robert J. El Niño, southern oscillation & climatic variability. CSIRO, 1996.

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6

Wright, Peter B. Relationships between surface observations over the global oceans and the southern oscillation. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, 1985.

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7

Kikuchi, Kazuyoshi. Data analysis studies on the propagation characteristics of the Madden-Julian Oscillation (MJO). Center for Climate System Research, University of Tokyo, 2006.

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8

Allan, Rob. El Niño Southern Oscillation and climatic variability. CSIRO PUblishing, 1996.

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9

Fiedler, Paul C. Seasonal climatologies and variability of eastern tropical Pacific surface waters. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Marine Fisheries Service, 1992.

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10

Giese, Benjamin S. Equatorial oceanic response to forcing on time scales from days to months. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Pacific Marine Environmental Laboratory, 1989.

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11

Western Pacific International Meeting and Workshop on TOGA COARE (1989 Centre ORSTOM de Nouméa). Proceedings of the Western Pacific International Meeting and Workshop on TOGA COARE, held at Centre ORSTOM de Nouméa, New Caledonia, May 24-30, 1989. Institut français de recherche scientifique pour le développement en coopération, Centre de Nouméa, 1989.

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12

Halpert, Michael S. Atlas of tropical sea surface temperature and surface winds. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Weather Service, 1989.

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13

Fiedler, Paul C. Seasonal Climatologies and variability of eastern tropical Pacific surface waters. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Marine Fisheries Service, 1992.

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14

Hayashi, Michiya. A modeling study on coupling between westerly wind events and ENSO. Division of Climate System Research, Atmosphere and Ocean Research Institute, The University of Tokyo, 2018.

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15

Wallace, John M. El Niño and climate prediction. National Oceanic and Atmosphere Administration, 1999.

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16

M, Wallace John. El Niño and climate prediction. [University Corporation for Atmospheric Research, Office for Interdisciplinary Earth Studies], 1994.

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17

National Research Council (U.S.). Advisory Panel for the Tropical Oceans and Global Atmosphere Program., ed. Learning to predict climate variations associated with El Niño and the southern oscillation: Accomplishments and legacies of the TOGA program. National Academy Press, 1996.

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18

The Role of Radiative Processes in the Tropical Intraseasonal Oscillation. Storming Media, 1997.

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19

Intraseasonal Variability in the Atmosphere-Ocean Climate System. Springer Berlin Heidelberg, 2005. http://dx.doi.org/10.1007/b138817.

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20

Lau, William K. M., and Duane E. Waliser. Intraseasonal Variability in the Atmosphere-Ocean Climate System. Springer, 2010.

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21

Lau, William K. M., and Duane E. Waliser. Intraseasonal Variability in the Atmosphere-Ocean Climate System. Springer London, Limited, 2007.

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22

Lau, William K. M., and Duane E. Waliser. Intraseasonal Variability in the Atmosphere-Ocean Climate System. Springer, 2012.

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23

Lau, William K. M., and Duane E. Waliser. Intraseasonal Variability in the Atmosphere-Ocean Climate System. Springer, 2013.

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24

Lau, William K. M., and Duane E. Waliser. Intraseasonal Variability in the Atmosphere-Ocean Climate System. Springer, 2009.

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25

Atmospheric model intercomparison project (AMIP): Intraseasonal oscillations in 15 atmospheric general circulation models (results from an AMIP diagnostic subproject). Joint Planning Staff for WCRP, World Meteorological Organization, 1995.

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26

Wang, Bin. Intraseasonal Modulation of the Indian Summer Monsoon. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.616.

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The strongest Indian summer monsoon (ISM) on the planet features prolonged clustered spells of wet and dry conditions often lasting for two to three weeks, known as active and break monsoons. The active and break monsoons are attributed to a quasi-periodic intraseasonal oscillation (ISO), which is an extremely important form of the ISM variability bridging weather and climate variation. The ISO over India is part of the ISO in global tropics. The latter is one of the most important meteorological phenomena discovered during the 20th century (Madden & Julian, 1971, 1972). The extreme dry an

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27

(Editor), Henry Frank Diaz, and Vera Markgraf (Editor), eds. El Niño: Historical and Paleoclimatic Aspects of the Southern Oscillation. Cambridge University Press, 1993.

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28

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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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 sta

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29

Dixit, Sanjay. Simulation of tropical pacific circulation anomalies with linear atmosphere and ocean models. 1987.

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30

Ahn, Joong Bae. A study of El Niño/southern oscillation: Numerical experiments and data analysis. 1990.

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31

(Editor), S. George Philander, James R. Holton (Series Editor), and Renata Dmowska (Series Editor), eds. El Nino, La Nina, and the Southern Oscillation, Volume 46 (International Geophysics). Academic Press, 1989.

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32

El Niño, La Niña, and the southern oscillation. Academic Press, 1990.

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33

Hameed, Saji N. The Indian Ocean Dipole. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.619.

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Discovered at the very end of the 20th century, the Indian Ocean Dipole (IOD) is a mode of natural climate variability that arises out of coupled ocean–atmosphere interaction in the Indian Ocean. It is associated with some of the largest changes of ocean–atmosphere state over the equatorial Indian Ocean on interannual time scales. IOD variability is prominent during the boreal summer and fall seasons, with its maximum intensity developing at the end of the boreal-fall season. Between the peaks of its negative and positive phases, IOD manifests a markedly zonal see-saw in anomalous sea surface

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34

Yang, Kun. Observed Regional Climate Change in Tibet over the Last Decades. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.587.

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The Tibetan Plateau (TP) is subjected to strong interactions among the atmosphere, hydrosphere, cryosphere, and biosphere. The Plateau exerts huge thermal forcing on the mid-troposphere over the mid-latitude of the Northern Hemisphere during spring and summer. This region also contains the headwaters of major rivers in Asia and provides a large portion of the water resources used for economic activities in adjacent regions. Since the beginning of the 1980s, the TP has undergone evident climate changes, with overall surface air warming and moistening, solar dimming, and decrease in wind speed.

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