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Books on the topic 'Midlatitude'

Author: Grafiati
Published: 4 June 2021
Last updated: 25 May 2024

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1

Lackmann, Gary. Midlatitude Synoptic Meteorology. Boston, MA: American Meteorological Society, 2011. http://dx.doi.org/10.1007/978-1-878220-56-1.

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2

Kintner, Paul M., Anthea J. Coster, Tim Fuller-Rowell, Anthony J. Mannucci, Michael Mendillo, and Roderick Heelis, eds. Midlatitude Ionospheric Dynamics and Disturbances. Washington, D. C.: American Geophysical Union, 2008. http://dx.doi.org/10.1029/gm181.

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3

Hoskins, Brian J., and Ian N. James. Fluid Dynamics of the Midlatitude Atmosphere. Chichester: John Wiley & Sons, Ltd, 2014. http://dx.doi.org/10.1002/9781118526002.

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4

Midlatitude synoptic meteorology: Dynamics, analysis, and forecasting. Boston, Mass: American Meteorological Society, 2011.

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5

Midlatitude Storm Track Response to Increased Greenhouse Warming. [New York, N.Y.?]: [publisher not identified], 2012.

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6

E, Graham Nicholas, California Energy Commission. Public Interest Energy Research., and Hydrologic Research Center, eds. Tropical Pacific midlatitude teleconnections in medieval times: PIER project report. [Sacramento, Calif.]: California Energy Commission, 2007.

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7

E, Graham Nicholas, California Energy Commission. Public Interest Energy Research., and Hydrologic Research Center, eds. Tropical Pacific midlatitude teleconnections in medieval times: PIER project report. [Sacramento, Calif.]: California Energy Commission, 2007.

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8

E, Graham Nicholas, California Energy Commission. Public Interest Energy Research., and Hydrologic Research Center, eds. Tropical Pacific midlatitude teleconnections in medieval times: PIER project report. [Sacramento, Calif.]: California Energy Commission, 2007.

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9

L, Killeen T., and United States. National Aeronautics and Space Administration., eds. Nocturnal observations of the semidiurnal tide at a midlatitude site. [Washington, DC: National Aeronautics and Space Administration, 1995.

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10

L, Killeen T., and United States. National Aeronautics and Space Administration., eds. Nocturnal observations of the semidiurnal tide at a midlatitude site. [Washington, DC: National Aeronautics and Space Administration, 1995.

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11

Graham, Nicholas E. Tropical Pacific midlatitude teleconnections in medieval times: PIER project report. Sacramento, Calif.]: California Energy Commission, 2007.

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12

Watanabe, Masahiro. Mechanisms of the decadal climate variability in the midlatitude atmosphere-ocean system. [Tokyo]: Center for Climate System Research, University of Tokyo, 2000.

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13

Mechanisms of the decadal climate variability in the midlatitude atmosphere-ocean system. Tokyo]: Center for Climate System Research, University of Tokyo, 2000.

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14

Jan, Paegle, and United States. National Aeronautics and Space Administration., eds. Impact of analysis uncertainty upon regional atmospheric moisture flux: [final report, 22 Sep. 1993 - 31 Dec. 1994]. [Washington, DC: National Aeronautics and Space Administration, 1995.

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15

1968-, Richardson Yvette, and Wiley online library, eds. Mesoscale meteorology in midlatitudes. Chichester, West Sussex: Wiley-Blackwell, 2010.

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16

Bluestein, Howard. Synoptic-dynamic meteorology in midlatitudes. New York: Oxford University Press, 1992.

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17

Bluestein, Howard B. Synoptic-dynamic meteorology in midlatitudes. New York: Oxford University Press, 1992.

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18

Lackmann, Gary. Midlatitude Synoptic Meteorology. American Meteorological Society, 2012.

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19

Polavarapu, Saroja Malu *. Midlatitude cyclones and cyclogenesis. 1990.

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20

M, Kintner Paul, ed. Midlatitude ionospheric dynamics and disturbances. Washington, DC: American Geophysical Union, 2008.

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21

Mendillo, Michael, Paul M. Kintner, Anthea J. Coster, Tim Fuller-Rowell, and Antony J. Mannucci. Midlatitude Ionospheric Dynamics and Disturbances. American Geophysical Union, 2013.

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22

Jr, Kintner Paul M., Michael Mendillo, Anthea J. Coster, Tim Fuller-Rowell, and Antony J. Mannucci. Midlatitude Ionospheric Dynamics and Disturbances. Wiley & Sons, Limited, John, 2013.

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23

Mendillo, Michael, Paul M. Kintner, Anthea J. Coster, Tim Fuller-Rowell, and Antony J. Mannucci. Midlatitude Ionospheric Dynamics and Disturbances. American Geophysical Union, 2013.

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24

Fluid Dynamics Of The Midlatitude Atmosphere. John Wiley and Sons Ltd, 2014.

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25

Fluid Dynamics Of The Midlatitude Atmosphere. John Wiley & Sons, 2012.

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26

National Aeronautics and Space Administration (NASA) Staff. Promis Series. Volume 8: Midlatitude Ground Magnetograms. Independently Published, 2018.

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27

MidLatitude Slope Deposits Cover Beds Developments in Sedimentology. Elsevier Science & Technology, 2013.

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28

Synoptic-Dynamic Meteorology: Visual Exercises to Complement Midlatitude Synoptic Meteorology. American Meteorological Society, 2012.

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29

National Aeronautics and Space Administration (NASA) Staff. Towards a Theory of Tropical/Midlatitude Mass Exchange from the Earth's Surface Through the Stratosphere. Independently Published, 2019.

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30

Markowski, Paul, and Yvette Richardson. Mesoscale Meteorology in Midlatitudes. Wiley & Sons, Incorporated, John, 2011.

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31

Markowski, Paul M., and Yvette P. Richardson. Mesoscale Meteorology in Midlatitudes. Wiley & Sons, Incorporated, John, 2010.

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32

Markowski, Paul, and Yvette Richardson. Mesoscale Meteorology in Midlatitudes. Wiley & Sons, Incorporated, John, 2011.

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33

Keng-Gaik, Lum. The influence of Large-scale 200 mb tropical divergence events on the midlatitude zonal flow over the Asia-Pacific region during the 1983-84 winter. 1985.

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34

Towards a theory of tropical/midlatitude mass exchange from the Earth's surface through the stratosphere: Progress report for year one, 12/1/94-9/30/95. [Washington, D.C: National Aeronautics and Space Administration, 1995.

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35

Towards a theory of tropical/midlatitude mass exchange from the Earth's surface through the stratosphere: Progress report for year one, 12/1/94-9/30/95. [Washington, D.C: National Aeronautics and Space Administration, 1995.

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36

Bluestein, Howard B. Synoptic-Dynamic Meteorology in Midlatitudes: Volume II: Observations and Theory of Weather Systems (Synoptic-Dynamic Meteorology in Midlatitudes). Oxford University Press, USA, 1993.

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37

Omstedt, Anders. The Development of Climate Science of the Baltic Sea Region. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.654.

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Dramatic climate changes have occurred in the Baltic Sea region caused by changes in orbital movement in the earth–sun system and the melting of the Fennoscandian Ice Sheet. Added to these longer-term changes, changes have occurred at all timescales, caused mainly by variations in large-scale atmospheric pressure systems due to competition between the meandering midlatitude low-pressure systems and high-pressure systems. Here we follow the development of climate science of the Baltic Sea from when observations began in the 18th century to the early 21st century. The question of why the water level is sinking around the Baltic Sea coasts could not be answered until the ideas of postglacial uplift and the thermal history of the earth were better understood in the 19th century and periodic behavior in climate related time series attracted scientific interest. Herring and sardine fishing successes and failures have led to investigations of fishery and climate change and to the realization that fisheries themselves have strongly negative effects on the marine environment, calling for international assessment efforts. Scientists later introduced the concept of regime shifts when interpreting their data, attributing these to various causes. The increasing amount of anoxic deep water in the Baltic Sea and eutrophication have prompted debate about what is natural and what is anthropogenic, and the scientific outcome of these debates now forms the basis of international management efforts to reduce nutrient leakage from land. The observed increase in atmospheric CO2 and its effects on global warming have focused the climate debate on trends and generated a series of international and regional assessments and research programs that have greatly improved our understanding of climate and environmental changes, bolstering the efforts of earth system science, in which both climate and environmental factors are analyzed together.Major achievements of past centuries have included developing and organizing regular observation and monitoring programs. The free availability of data sets has supported the development of more accurate forcing functions for Baltic Sea models and made it possible to better understand and model the Baltic Sea–North Sea system, including the development of coupled land–sea–atmosphere models. Most indirect and direct observations of the climate find great variability and stochastic behavior, so conclusions based on short time series are problematic, leading to qualifications about periodicity, trends, and regime shifts. Starting in the 1980s, systematic research into climate change has considerably improved our understanding of regional warming and multiple threats to the Baltic Sea. Several aspects of regional climate and environmental changes and how they interact are, however, unknown and merit future research.
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38

Nash, David. Changes in Precipitation Over Southern Africa During Recent Centuries. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.539.

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Precipitation levels in southern Africa exhibit a marked east–west gradient and are characterized by strong seasonality and high interannual variability. Much of the mainland south of 15°S exhibits a semiarid to dry subhumid climate. More than 66 percent of rainfall in the extreme southwest of the subcontinent occurs between April and September. Rainfall in this region—termed the winter rainfall zone (WRZ)—is most commonly associated with the passage of midlatitude frontal systems embedded in the austral westerlies. In contrast, more than 66 percent of mean annual precipitation over much of the remainder of the subcontinent falls between October and March. Climates in this summer rainfall zone (SRZ) are dictated by the seasonal interplay between subtropical high-pressure systems and the migration of easterly flows associated with the Intertropical Convergence Zone. Fluctuations in both SRZ and WRZ rainfall are linked to the variability of sea-surface temperatures in the oceans surrounding southern Africa and are modulated by the interplay of large-scale modes of climate variability, including the El Niño-Southern Oscillation (ENSO), Southern Indian Ocean Dipole, and Southern Annular Mode.Ideas about long-term rainfall variability in southern Africa have shifted over time. During the early to mid-19th century, the prevailing narrative was that the climate was progressively desiccating. By the late 19th to early 20th century, when gauged precipitation data became more readily available, debate shifted toward the identification of cyclical rainfall variation. The integration of gauge data, evidence from historical documents, and information from natural proxies such as tree rings during the late 20th and early 21st centuries, has allowed the nature of precipitation variability since ~1800 to be more fully explored.Drought episodes affecting large areas of the SRZ occurred during the first decade of the 19th century, in the early and late 1820s, late 1850s–mid-1860s, mid-late 1870s, earlymid-1880s, and mid-late 1890s. Of these episodes, the drought during the early 1860s was the most severe of the 19th century, with those of the 1820s and 1890s the most protracted. Many of these droughts correspond with more extreme ENSO warm phases.Widespread wetter conditions are less easily identified. The year 1816 appears to have been relatively wet across the Kalahari and other areas of south central Africa. Other wetter episodes were centered on the late 1830s–early 1840s, 1855, 1870, and 1890. In the WRZ, drier conditions occurred during the first decade of the 19th century, for much of the mid-late 1830s through to the mid-1840s, during the late 1850s and early 1860s, and in the early-mid-1880s and mid-late 1890s. As for the SRZ, markedly wetter years are less easily identified, although the periods around 1815, the early 1830s, mid-1840s, mid-late 1870s, and early 1890s saw enhanced rainfall. Reconstructed rainfall anomalies for the SRZ suggest that, on average, the region was significantly wetter during the 19th century than the 20th and that there appears to have been a drying trend during the 20th century that has continued into the early 21st. In the WRZ, average annual rainfall levels appear to have been relatively consistent between the 19th and 20th centuries, although rainfall variability increased during the 20th century compared to the 19th.
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