Книги: "Tropical lakes"

1

The ecology of tropical lakes and rivers. Chichester [West Sussex]: Wiley, 1986.

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2

International Workshop on Restoration and Management of Eutrophic Lakes (2001 Kunming Shi, China). Restoration and management of tropical eutrophic lakes. Edited by Reddy M. V. Enfield, NH: Science Publishers, 2005.

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3

J, Lemoalle, ed. Ecological dynamics of tropical inland waters. Cambridge: Cambridge University Press, 1998.

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4

Westgate, James W. After the dinosaurs: A Texas tropical paradise recovered at Lake Casa Blanca. Austin, Tex: Texas Parks and Wildlife Press, 1999.

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5

Sharma, U. P. Ecology, conservation, and management of Kawar Lake: A major tropical wetland of South East Asia. Bhagalpur: U.P. Sharma, 1995.

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6

M, Harper David, ed. Lake Naivasha, Kenya: Papers submitted by participants at the conference "Science and the Sustainable Management of Shallow Tropical Waters" held at Kenya Wildlife Services Training Institute, Naivasha, Kenya, 11-16 April 1999, together with those from additional studies on the lake. Dordrecht: Kluwer Academic Publishers, 2003.

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7

Beattie, Keith. Establishing a scientific basis for reconstructing the tropic status of a lake using blue-green algal pigments in the lake sediment cores. [S.l: The Author], 1996.

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8

Gosline, G., ed. Flora of West Tropical Africa: All Territories in West Africa South of Latitude 18° N. and to the West of Lake Chad, and Fernando Po. London, UK: Royal Botanic Gardens Kew, 2014.

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9

Vincent, Warwick F. Lakes: A Very Short Introduction. Oxford University Press, 2018. http://dx.doi.org/10.1093/actrade/9780198766735.001.0001.

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From the mysterious depths of Lake Vostok, Antarctica, to tropical floodplain lakes, inland seas, hydro-reservoirs, and numerous waterbodies in our local environment, lakes encompass a huge diversity of shapes, sizes, depths, colours, and even salinities. Lakes are important, unique ecosystems, providing us with drinking water and food. Lakes: A Very Short Introduction introduces lake science (‘limnology’), discussing the importance of sustaining these complex ecosystems; and the impact on lake biodiversity of features such as climate, seasons, salinity, and sedimentation. It traces the origins of lake science from François Forel’s seminal work on Lake Geneva to modern approaches, such as environmental sensors, satellite observations, stable isotope analysis, and DNA-based technologies.

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10

Payne, A. I. The Ecology of Tropical Lakes and Rivers. John Wiley and Sons Ltd, 1991.

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11

Reddy, M. V. Restoration and Management of Tropical Eutrophic Lakes. Taylor & Francis Group, 2005.

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12

INTERNATIONAL WORKSHOP ON RESTORATION AN. Restoration And Mangement Of Tropical Eutropic Lakes. Science Publishers, 2005.

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13

Reddy, M. V. Restoration and Management of Tropical Eutrophic Lakes. Taylor & Francis Group, 2005.

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14

Lévêque, C., J. P. Carmouze, and J. R. Durant. Lake Chad: Ecology and Productivity of a Shallow Tropical Ecosystem. Springer, 2012.

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15

Lévêque, C., J. P. Carmouze, and J. R. Durant. Lake Chad: Ecology and Productivity of a Shallow Tropical Ecosystem. Springer, 2012.

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16

Lake Chad: Ecology and Productivity of a Shallow Tropical Ecosystem. Springer, 2012.

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17

Thornton, J. A. Lake Mcilwaine: The Eutrophication and Recovery of a Tropical African Man-Made Lake. Springer, 2012.

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18

Thornton, J. A. Lake Mcilwaine: The Eutrophication and Recovery of a Tropical African Man-Made Lake. Ingramcontent, 2011.

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19

Lézine, Anne-Marie. Vegetation at the Time of the African Humid Period. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.530.

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An orbitally induced increase in summer insolation during the last glacial-interglacial transition enhanced the thermal contrast between land and sea, with land masses heating up compared to the adjacent ocean surface. In North Africa, warmer land surfaces created a low-pressure zone, driving the northward penetration of monsoonal rains originating from the Atlantic Ocean. As a consequence, regions today among the driest of the world were covered by permanent and deep freshwater lakes, some of them being exceptionally large, such as the “Mega” Lake Chad, which covered some 400 000 square kilometers. A dense network of rivers developed.What were the consequences of this climate change on plant distribution and biodiversity? Pollen grains that accumulated over time in lake sediments are useful tools to reconstruct past vegetation assemblages since they are extremely resistant to decay and are produced in great quantities. In addition, their morphological character allows the determination of most plant families and genera.In response to the postglacial humidity increase, tropical taxa that survived as strongly reduced populations during the last glacial period spread widely, shifting latitudes or elevations, expanding population size, or both. In the Saharan desert, pollen of tropical trees (e.g., Celtis) were found in sites located at up to 25°N in southern Libya. In the Equatorial mountains, trees (e.g., Olea and Podocarpus) migrated to higher elevations to form the present-day Afro-montane forests. Patterns of migration were individualistic, with the entire range of some taxa displaced to higher latitudes or shifted from one elevation belt to another. New combinations of climate/environmental conditions allowed the cooccurrences of taxa growing today in separate regions. Such migrational processes and species-overlapping ranges led to a tremendous increase in biodiversity, particularly in the Saharan desert, where more humid-adapted taxa expanded along water courses, lakes, and wetlands, whereas xerophytic populations persisted in drier areas.At the end of the Holocene era, some 2,500 to 4,500 years ago, the majority of sites in tropical Africa recorded a shift to drier conditions, with many lakes and wetlands drying out. The vegetation response to this shift was the overall disruption of the forests and the wide expansion of open landscapes (wooded grasslands, grasslands, and steppes). This environmental crisis created favorable conditions for further plant exploitation and cereal cultivation in the Congo Basin.

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20

Talling, Jack F., and Jacques Lemoalle. Ecological Dynamics of Tropical Inland Waters. Cambridge University Press, 2011.

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21

Darchambeau, François, Martin Schmid, and Jean-Pierre Descy. Lake Kivu: Limnology and Biogeochemistry of a Tropical Great Lake. Springer London, Limited, 2012.

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22

Lake Kivu Limnology And Biogeochemistry Of A Tropical Great Lake. Springer, 2012.

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23

Darchambeau, François, Martin Schmid, and Jean-Pierre Descy. Lake Kivu: Limnology and Biogeochemistry of a Tropical Great Lake. Springer Netherlands, 2014.

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24

Lake Alchichica Limnology: The Uniqueness of a Tropical Maar Lake. Springer International Publishing AG, 2021.

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25

Kalk, M., A. J. McLachlan, and C. Howard-Williams. Lake Chilwa: Studies of Change in a Tropical Ecosystem. Springer London, Limited, 2012.

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26

(Editor), M. Kalk, C. Howard-Williams (Editor), and A. J. McLachlan (Editor), eds. Lake Chilwa: Studies of Change in a Tropical Ecosystem (Monographiae Biologicae). Springer, 2007.

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27

Jacobsen, Dean, and Olivier Dangles. The waterscape at high altitudes. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198736868.003.0002.

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Chapter 2 presents the amazing variety of running waters, lakes, ponds, and wetlands found at high altitudes. These waterbodies are not equally distributed among the world’s high altitude places, but tend to be concentrated in certain areas, primarily determined by regional climate and topography. Thus, a large proportion of the world’s truly high altitude aquatic systems are found at lower latitudes, mostly in the tropics. The chapter presents general patterns in the geographical distribution of high altitude waters, and gives examples of some of the most extreme systems. High altitude aquatic systems and habitats cover a broad variety in dynamics and physical appearance. These differences may be related to, for example, water source (glacier-fed, rain-fed, or groundwater-fed streams), geological origin (e.g. glacial, volcanic, or tectonic lakes), or catchment slope and altitude (different types of peatland wetlands). This is exemplified and richly illustrated through numerous photos.

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28

Balon, E. K., and A. G. Coche. Lake Kariba: A Man-Made Tropical Ecosystem in Central Africa. Ingramcontent, 2012.

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29

Coche, A. G., and E. K. Balon. Lake Kariba: A Man-Made Tropical Ecosystem in Central Africa. Springer, 2012.

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30

Thompson, Lonnie G., and Alan L. Kolata. Twelfth Century AD. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199329199.003.0008.

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Climate is a fundamental and independent variable of human existence. Given that 50 percent of the Earth’s surface and much of its population exist between 30oN and 30oS, paleoenvironmental research in the Earth’s tropical regions is vital to our understanding of the world’s current and past climate change. Most of the solar energy that drives the climate system is absorbed in these regions. Paleoclimate records reveal that tropical processes, such as variations in the El Niño-Southern Oscillation (ENSO), have affected the climate over much of the planet. Climatic variations, particularly in precipitation and temperature, play a critical role in the adaptations of agrarian cultures located in zones of environmental sensitivity, such as those of the coastal deserts, highlands, and altiplano of the Andean region. Paleoclimate records from the Quelccaya ice cap (5670 masl) in highland Peru that extend back ~1800 years show good correlation between precipitation and the rise and fall of pre-Hispanic civilizations in western Peru and Bolivia. Sediment cores extracted from Lake Titicaca provide independent evidence of this correspondence with particular reference to the history of the pre-Hispanic Tiwanaku state centered in the Andean altiplano. Here we explore, in particular, the impacts of climate change on the development and ultimate dissolution of this altiplano state.

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31

Review of Tropical Reservoirs and Their Fisheries: The Cases of Lake Nasser, Lake Volta and Indo-Gangetic Basin Reservoir. Rowman & Littlefield Publishers, Incorporated, 2013.

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32

Haynes, Skip. Lake Shore Drive: Stories of the Road and Tales of the Tropicana. BookBaby, 2017.

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33

Harper, David M., M. Everard, R. Boar, and P. Hickley. Lake Naivasha, Kenya: Papers Submitted by Participants at the Conference Science and the Sustainable Management of Shallow Tropical Waters Held at Kenya Wildlife Services Training Institute, Naivasha, Kenya, 11-16 April 1999, Together with Those from Additional Studies on the Lake. Springer Netherlands, 2011.

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34

Harper, David M., M. Everard, R. Boar, and P. Hickley. Lake Naivasha, Kenya: Papers Submitted by Participants at the Conference Science and the Sustainable Management of Shallow Tropical Waters Held at Kenya Wildlife Services Training Institute, Naivasha, Kenya, 11-16 April 1999, Together with Those from Additional Studies on the Lake. Springer London, Limited, 2013.

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35

Schiemer, F. Limnology of Parakrama Samudra -- Sri Lanka: A Case Study of an Ancient Man-Made Lake in the Tropics. Springer, 2012.

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36

Schiemer, F. Limnology of Parakrama Samudra -- Sri Lanka: A Case Study of an Ancient Man-Made Lake in the Tropics. Springer Netherlands, 2011.

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37

Schiemer, F. Limnology of Parakrama Samudra - Sri Lanka: A Case Study of an Ancient Manmade Lake in the Tropics (Developments in Hydrobiology). Springer, 2007.

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38

Memories, Forever. Visitors Guestbook: Tropical Jungle Animals Guest Signing Book - Address Contact Message Log Tracker Recorder Address Lines - Lake Country Vacation House Registry - Cabin Welcome Guesthouse Lodge Holiday Beach Home-Feedback Comments Ledger Business Record. Independently Published, 2019.

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39

100 Easy Pages - Adult Coloring Book - Flowers, Mandalas, Animals, Birds, Butterflies, Cats, Dogs, Horses, Owls, Lion, Wolf, Fish, Lake, River, Sea, Ocean, Lighthouse, Travel, Love, Valentine, Heart, Winter, Summer, Tropical, Easter, Halloween and Christmas. Independently Published, 2020.

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40

Artworks, Autumn Season. 100 Easy Pages - Adult Coloring Book - Flowers, Mandalas, Animals, Birds, Butterflies, Cats, Dogs, Horses, Owls, Lion, Wolf, Fish, Lake, River, Sea, Ocean, Lighthouse, Travel, Love, Valentine, Heart, Winter, Summer, Tropical, Easter, Halloween and Christmas. Independently Published, 2021.

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41

Books, Stress Relieving Coloring. 100 Easy Pages - Adult Coloring Book - Flowers, Mandalas, Animals, Birds, Butterflies, Cats, Dogs, Horses, Owls, Lion, Wolf, Fish, Lake, River, Sea, Ocean, Lighthouse, Travel, Love, Valentine, Heart, Winter, Summer, Tropical, Easter, Halloween and Christmas. Independently Published, 2020.

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42

Petals & Pastels Coloring Books. 100 Easy Pages - Adult Coloring Book - Flowers, Mandalas, Animals, Birds, Butterflies, Cats, Dogs, Horses, Owls, Lion, Wolf, Fish, Lake, River, Sea, Ocean, Lighthouse, Travel, Love, Valentine, Heart, Winter, Summer, Tropical, Easter, Halloween and Christmas. Independently Published, 2020.

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43

Artworks, Awesome. 100 Easy Pages - Adult Coloring Book - Flowers, Mandalas, Animals, Birds, Butterflies, Cats, Dogs, Horses, Owls, Lion, Wolf, Fish, Lake, River, Sea, Ocean, Lighthouse, Travel, Love, Valentine, Heart, Winter, Summer, Tropical, Easter, Halloween and Christmas. Independently Published, 2021.

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44

Artworks, Amazing. 100 Easy Pages - Adult Coloring Book - Flowers, Mandalas, Animals, Birds, Butterflies, Cats, Dogs, Horses, Owls, Lion, Wolf, Fish, Lake, River, Sea, Ocean, Lighthouse, Travel, Love, Valentine, Heart, Winter, Summer, Tropical, Easter, Halloween and Christmas. Independently Published, 2021.

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45

100 Easy Pages - Adult Coloring Book - Flowers, Mandalas, Animals, Birds, Butterflies, Cats, Dogs, Horses, Owls, Lion, Wolf, Fish, Lake, River, Sea, Ocean, Lighthouse, Travel, Love, Valentine, Heart, Winter, Summer, Tropical, Easter, Halloween and Christmas. Independently Published, 2020.

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46

Adults, Stress Relieving For. 100 Easy Pages - Adult Coloring Book - Flowers, Mandalas, Animals, Birds, Butterflies, Cats, Dogs, Horses, Owls, Lion, Wolf, Fish, Lake, River, Sea, Ocean, Lighthouse, Travel, Love, Valentine, Heart, Winter, Summer, Tropical, Easter, Halloween and Christmas. Independently Published, 2020.

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47

Norrgård, Stefan. Changes in Precipitation Over West Africa During Recent Centuries. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.536.

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Water, not temperature, governs life in West Africa, and the region is both temporally and spatially greatly affected by rainfall variability. Recent rainfall anomalies, for example, have greatly reduced crop productivity in the Sahel area. Rainfall indices from recent centuries show that multidecadal droughts reoccur and, furthermore, that interannual rainfall variations are high in West Africa. Current knowledge of historical rainfall patterns is, however, fairly limited. A detailed rainfall chronology of West Africa is currently only available from the beginning of the 19th century. For the 18th century and earlier, the records are still sporadic, and an interannual rainfall chronology has so far only been obtained for parts of the Guinea Coast. Thus, there is a need to extend the rainfall record to fully understand past precipitation changes in West Africa.The main challenge when investigating historical rainfall variability in West Africa is the scarcity of detailed and continuous data. Readily available meteorological data barely covers the last century, whereas in Europe and the United States for example, the data sometimes extend back two or more centuries. Data availability strongly correlates with the historical development of West Africa. The strong oral traditions that prevailed in the pre-literate societies meant that only some of the region’s history was recorded in writing before the arrival of the Europeans in the 16th century. From the 19th century onwards, there are, therefore, three types of documents available, and they are closely linked to the colonization of West Africa. These are: official records started by the colonial governments continuing to modern day; regular reporting stations started by the colonial powers; and finally, temporary nongovernmental observations of various kinds. For earlier periods, the researcher depends on noninstrumental observations found in letters, reports, or travel journals made by European slave traders, adventurers, and explorers. Spatially, these documents are confined to the coastal areas, as Europeans seldom ventured inland before the mid-1800s. Thus, the inland regions are generally poorly represented. Arabic chronicles from the Sahel provide the only source of information, but as historical documents, they include several spatiotemporal uncertainties. Climate researchers often complement historical data with proxy-data from nature’s own archives. However, the West African environment is restrictive. Reliable proxy-data, such as tree-rings, cannot be exploited effectively. Tropical trees have different growth patterns than trees in temperate regions and do not generate growth rings in the same manner. Sediment cores from Lake Bosumtwi in Ghana have provided, so far, the best centennial overview when it comes to understanding precipitation patterns during recent centuries. These reveal that there have been considerable changes in historical rainfall patterns—West Africa may have been even drier than it is today.

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Книги з теми "Tropical lakes"

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