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Books on the topic 'ENSO'

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Author: Grafiati

Published: 4 June 2021

Last updated: 6 July 2024

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1

Suzuki, Kōji. Enso-kun kisha ni noru. Tōkyō: Fukuinkan Shoten, 1986.

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2

Suzuki, Kōji. Enso-kun kisha ni noru. Tōkyō: Fukuinkan Shoten, 1990.

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3

United States. National Weather Service. El Niño, La Niña, and ENSO. Silver Spring, Md.]: National Weather Service, 2006.

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4

United States. National Weather Service. El Niño, La Niña, and ENSO. Silver Spring, Md.]: National Weather Service, 2007.

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5

Mononen, Paula. Enso-Gutzeit Oy:n pankakosken kartonkitehtaan erityishaittavaikutukset Lieksanjoessa. Helsinki: Vesi- ja ympäristöhallitus, Pohjois-Karjalan vesi- ja ympäristöpiiri, 1989.

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6

Bells, Youlsau. 2002/03 el Niño/ENSO national action plan. [Koror, Republic of Palau: Mitigation Committee, 2001.

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7

Rytteri, Teijo. Metsäteollisuusyrityksen luonto: Tutkimus Enso-Gutzeitin ympäristö- ja yhteiskuntavastuun muotoutumisesta. Joensuu: Joensuun yliopisto, Maantieteen laitos, 2002.

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8

Kuman, Tony. Report on ENSO workshop, Nadi, Fiji, 19th-24th October 1999. Papua New Guinea: Office of Environment & Conservation, Environment Division, 1999.

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9

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

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10

Jong, Bor-Ting. Seasonality and Regionality of ENSO Teleconnections and Impacts on North America. [New York, N.Y.?]: [publisher not identified], 2019.

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11

Houseago, Richenda Elouise. The teleconnections between ENSO and the climate variability of the Antarctica. Birmingham: University of Birmingham, 1998.

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12

Kohtanen, Jukka. Työtaistelut ja neuvottelusuhteet Enso-Gutzeit Oy:n Kotkan tehtailla vuosina 1971-84. Helsinki: Työelämän suhteiden neuvottelukunta, 1987.

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13

ENSO yu hai yang huan jing he Zhongguo qi hou yi chang. Beijing: Ke xue chu ban she, 2013.

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14

Sangyōkyoku, Japan Kinki Tsūshō. Heisei 2-nendo torikuroroechiren tō yūki enso kagōbutsu shiyō jittai chōsa hōkokusho. [Osaka]: Kinki Tsūshō Sangyōkyoku, 1991.

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15

Takau, Etisoni I. The climatological database of Tonga with its trends and relation to ENSO. Townsville, Australia: Physics Dept., James Cook University of North Queensland, 1992.

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16

Karonen, Petri. Enso-Gutzeit Oy laivanvarustajana: Oy Finnlines Ltd ja Merivienti Oy vuosina 1947-1982. Imatra: Enso-Gutzeit, 1992.

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17

Hamnett, Michael P. Impact of ENSO events on tuna fisheries in the U.S. affiliated Pacific Islands. [Honolulu, Hawaii: University of Hawaii, Joint Institute for Marine and Atmospheric Research, 2000.

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18

He, Yuxiang. A precipitation climatology for stations in the tropical Pacific basin: Effects of ENSO. [Washington, D.C.]: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Weather Service, 1998.

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19

He, Yuxiang. A precipitation climatology for stations in the tropical Pacific Basin: Effects of ENSO. [Silver Spring, Md.?]: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Weather Service, 1998.

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20

Marc de Ferrière Le Vayer. Les cinq vies de Corbehem: De Béghin à Stora Enso, l'histoire d'une usine. Douai: Pagine, 1998.

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21

International Symposium on Former ENSO Phenomena in Western South America: Records of El Niño Events (1992 Lima, Peru). Paleo-ENSO records: International symposium : extended abstracts : volume prepared for the International Symposium on Former ENSO Phenomena in Western South America--Records of El Niño Events, Lima 4-7 March, 1992. Lima: ORSTOM Lima, 1992.

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22

Griffiths, Gareth. The polemical Aalto: The Enso-Gutzeit headquarters, Helsinki (1959-1962) by Alvar Aalto : a formal analysis. Tampere: Tampere University of Technology, 1997.

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23

George C. Marshall Space Flight Center., ed. Statistical aspects of ENSO events (1950-1997) and the El Niño-Atlantic intense hurricane activity relationship. [Marshall Space Flight Center, Ala.]: National Aeronautics and Space Administration, George C. Marshall Space Flight Center, 1998.

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24

Lluch-Cota, Daniel B. Empirical investigation on the relationship between climate and small pelagic global regimes and El Niño - Southern oscillation (ENSO). Rome: Food and Agriculture Organization of the United Nations, 1997.

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25

Ensor, James. Ensor: James (art) Ensor. Paris: Réunion des musées nationaux, 2009.

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26

Laurence, Madeline, Swinbourne Anna, Musée d'Orsay, and Museum of Modern Art (New York, N.Y.), eds. Ensor: James (art) Ensor. Paris: Réunion des musées nationaux, 2009.

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27

Gisèle, Ollinger-Zinque, and Musées royaux des beaux-arts de Belgique., eds. Ensor. Wommelgem: Blondé Artprinting International, 1999.

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28

Griffiths, Jonathan, Elli Gillic, and Dushica Labovich. Enso. Independently Published, 2017.

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29

Enso. Entre Rios Books, 2020.

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30

Griffiths, Jonathan, Elli Gillic, and Dushica Labovich. Enso. Independently Published, 2013.

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31

Griffiths, Jonathan. Enso. Independently Published, 2017.

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32

Enso House. Abiding Nowhere Press, 2013.

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33

Chowdary, Jasti S., Anant Parekh, and C. Gnanaseelan. Indian Summer Monsoon: ENSO and Non-ENSO Teleconnections. Elsevier, 2021.

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34

Nicholls. Enso: Agrcltrl Fisheries. University of Cambridge ESOL Examinations, 2000.

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35

DeLaFont, Enso. Enso Circle: Zen Enso Circle, Represents Enlightenment, Strength, Elegance, the Universe and Emptiness. Independently Published, 2019.

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36

Seo, Audrey Yoshiko, and John Daido Loori. Enso: Zen Circles of Enlightenment. Weatherhill, 2009.

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37

Bailey, Michael. Enso: A Connection of Fables. CreateSpace Independent Publishing Platform, 2016.

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38

Enso: Zen Circles of Enlightenment. Weatherhill, 2007.

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39

Watson, Jacob. Enso Morning: Daily Meditation Gifts. Hunt Publishing Limited, John, 2016.

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40

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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41

National Aeronautics and Space Administration (NASA) Staff. On the Bimodality of Enso Cycle Extremes. Independently Published, 2018.

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42

National Aeronautics and Space Administration (NASA) Staff. On the Bimodality of Enso Cycle Extremes. Independently Published, 2018.

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43

Kucharski, Fred, and Muhammad Adnan Abid. Interannual Variability of the Indian Monsoon and Its Link to ENSO. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.615.

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The interannual variability of Indian summer monsoon is probably one of the most intensively studied phenomena in the research area of climate variability. This is because even relatively small variations of about 10% to 20% from the mean rainfall may have dramatic consequences for regional agricultural production. Forecasting such variations months in advance could help agricultural planning substantially. Unfortunately, a perfect forecast of Indian monsoon variations, like any other regional climate variations, is impossible in a long-term prediction (that is, more than 2 weeks or so in advance). The reason is that part of the atmospheric variations influencing the monsoon have an inherent predictability limit of about 2 weeks. Therefore, such predictions will always be probabilistic, and only likelihoods of droughts, excessive rains, or normal conditions may be provided. However, even such probabilistic information may still be useful for agricultural planning. In research regarding interannual Indian monsoon rainfall variations, the main focus is therefore to identify the remaining predictable component and to estimate what fraction of the total variation this component accounts for. It turns out that slowly varying (with respect to atmospheric intrinsic variability) sea-surface temperatures (SSTs) provide the dominant part of the predictable component of Indian monsoon variability. Of the predictable part arising from SSTs, it is the El Niño Southern Oscillation (ENSO) that provides the main part. This is not to say that other forcings may be neglected. Other forcings that have been identified are, for example, SST patterns in the Indian Ocean, Atlantic Ocean, and parts of the Pacific Ocean different from the traditional ENSO region, and springtime snow depth in the Himalayas, as well as aerosols. These other forcings may interact constructively or destructively with the ENSO impact and thus enhance or reduce the ENSO-induced predictable signal. This may result in decade-long changes in the connection between ENSO and the Indian monsoon. The physical mechanism for the connection between ENSO and the Indian monsoon may be understood as large-scale adjustment of atmospheric heatings and circulations to the ENSO-induced SST variations. These adjustments modify the Walker circulation and connect the rising/sinking motion in the central-eastern Pacific during a warm/cold ENSO event with sinking/rising motion in the Indian region, leading to reduced/increased rainfall.

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44

Ren, Hong-Li, Tao Lian, Michiya Hayashi, Ruihuang Xie, and Wenjun Zhang, eds. ENSO Nonlinearity and Complexity: Features, Mechanisms, Impacts and Prediction. Frontiers Media SA, 2022. http://dx.doi.org/10.3389/978-2-88976-725-0.

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45

El Niño Southern Oscillation (ENSO) effects on fisheries and aquaculture. FAO, 2020. http://dx.doi.org/10.4060/ca8348en.

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46

DeLaFont, Enso. Enso Circle with Great Wave of Kanagawa: This Enso Circle, Represents Enlightenment, Elegance, the Universe and Emptiness with the Strength of the Great Wave. Independently Published, 2019.

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47

Chowdhury, Rashed. Seasonal Flood Forecasts and Warning Response Opportunities: ENSO Applications in Bangladesh. Springer International Publishing AG, 2022.

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48

Schmid, Hans Bernhard, Michael Schmitz, and Beatrice Kobow. Background of Social Reality: Selected Contributions from the Inaugural Meeting of ENSO. Springer London, Limited, 2013.

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49

DeLaFont, Enso. Enso Circle with Great Wave of Kanagawa: 120 Pages of 6x9 Inches. Independently Published, 2019.

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50

Steiger, Diego. Bamboo Japanese Enso Circle Calendar 2022: Annual Calendar for Nature Lovers and Environmentalists. Independently Published, 2021.

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