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1

Smolka, Peter. Southern Hemisphere paleo- and neoclimates: Key sites, methods, data and models. Springer, 2000.

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2

Kousky, Vernon E. Atlas of Southern Hemisphere 500 mb teleconnection patterns derived from National Meteorological Center analyses. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Weather Service, 1992.

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3

Linacre, Edward. Climates and weather explained: An introduction from a southern perspective. Routledge, 1996.

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4

Linacre, Edward. Climates and Weather Explained. Taylor & Francis Inc, 2003.

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5

Linacre, Edward. Climates and weather explained. Routledge, 1997.

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6

Smirnov, N. P. Cikloničeskie centry dejstvija atmosfery Južnogo polušarija i izmenenija klimata =: Cyclonic action centres in the Southern hemisphere and climatic variations. RGGMU, 2004.

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7

Climate change: Developing southern hemisphere perspectives. Wiley, 1996.

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8

(Editor), Thomas W. Giambelluca, and Ann Henderson-Sellers (Editor), eds. Climate Change: Developing Southern Hemisphere Perspectives (Research & Developments in Climate & Climatology). Wiley, 1996.

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9

(Editor), Peter Smolka, and Wolfgang Volkheimer (Editor), eds. Southern Hemisphere Paleo- and Neoclimates: Key Sites, Methods, Data and Models. Springer, 2000.

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10

Climate succession and glacial history of the Southern Hemisphere over the past five million years. Australian Antarctic Division, 1995.

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11

van den Dool, Huug. Empirical Methods in Short-Term Climate Prediction. Oxford University Press, 2006. http://dx.doi.org/10.1093/oso/9780199202782.001.0001.

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This clear and accessible text describes the methods underlying short-term climate prediction at time scales of 2 weeks to a year. Although a difficult range to forecast accurately, there have been several important advances in the last ten years, most notably in understanding ocean-atmosphere interaction (El Nino for example), the release of global coverage data sets, and in prediction methods themselves. With an emphasis on the empirical approach, the text covers in detail empirical wave propagation, teleconnections, empirical orthogonal functions, and constructed analogue. It also provides
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12

Lindesay, J. A., Howard A. Bridgman, and John Jack Hobbs. Climates of the Southern Continents: Present, Past and Future. Wiley & Sons, Incorporated, John, 2000.

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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 widespre
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14

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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15

Holmes, Jonathan, and Philipp Hoelzmann. The Late Pleistocene-Holocene African Humid Period as Evident in Lakes. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.531.

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From the end of the last glacial stage until the mid-Holocene, large areas of arid and semi-arid North Africa were much wetter than present, during the interval that is known as the African Humid Period (AHP). During this time, large areas were characterized by a marked increase in precipitation, an expansion of lakes, river systems, and wetlands, and the spread of grassland, shrub land, and woodland vegetation into areas that are currently much drier. Simulations with climate models indicate that the AHP was the result of orbitally forced increase in northern hemisphere summer insolation, whi
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16

Tibaldi, Stefano, and Franco Molteni. Atmospheric Blocking in Observation and Models. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.611.

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The atmospheric circulation in the mid-latitudes of both hemispheres is usually dominated by westerly winds and by planetary-scale and shorter-scale synoptic waves, moving mostly from west to east. A remarkable and frequent exception to this “usual” behavior is atmospheric blocking. Blocking occurs when the usual zonal flow is hindered by the establishment of a large-amplitude, quasi-stationary, high-pressure meridional circulation structure which “blocks” the flow of the westerlies and the progression of the atmospheric waves and disturbances embedded in them. Such blocking structures can hav
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17

Clarke, Andrew. Temperature and diversity. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199551668.003.0015.

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The diversity (species richness) of plants and animals is typically highest in the tropics and the strongest environmental correlate of species richness is often climate. The energy for plant production is sunlight, but the rate is governed jointly by temperature and the availability of water (as captured by actual evapotranspiration, AET). Greater production is then linked to higher diversity because larger population size protects against stochastic extinction (the more individuals mechanism). A greater biomass and diversity of plants allows for a greater diversity of herbivores and so on th
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