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Książki na temat „Rainfall intensity”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 25 lipca 2025

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1

Hogg, W. D. Rainfall intensity-duration frequency values for Canadian locations. Environment Canada, Atmospheric Environment Service, 1989.

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2

Purvis, John C. Maximum rainfall intensity in South Carolina by county. South Carolina State Climatology Office, 1988.

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3

Toronto, University of, ed. Rainfall intensity-duration-frequency curves for Ontario locations. University of Toronto, 1985.

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4

E, Dowling Norman, and Langley Research Center, eds. Verification of rain-flow reconstructions of a variable amplitude load history. National Aeronautics and Space Administration, Langley Research Center, 1992.

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5

E, Dowling Norman, and Langley Research Center, eds. Verification of rain-flow reconstructions of a variable amplitude load history. National Aeronautics and Space Administration, Langley Research Center, 1992.

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6

Magni, Nelson Luiz Goi. Precipitações intensas no estado de São Paulo. Centro Tecnológico de Hidráulica, Departamento de Aguas e Energia Elétrica, Escola Politécnica da Universidade de São Paulo, 1986.

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7

Zahar, Yadh. Eléments d'hydrologie pour l'aménagement: Modélisation spatiale et temporelle des précipitations extrêmes et érosives en Tunisie centrale. Université des lettres, des arts et des sciences humaines, Tunis I, Faculté des lettres de la Manouba, 1997.

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8

Min-ho, Yi. Kangu kwanch'ŭk chŏnghwakto hyangsang e kwanhan yŏn'gu: Study for improvement of rainfall measurement accuracy. Kukt'o Haeyangbu Han'gang Hongsu T'ongjeso, 2010.

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9

Air Resources Laboratory (U.S.), ed. Precipitation frequency and intensity at the Idaho National Engineering Laboratory. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Air Resources Laboratory, 1996.

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10

Khaladkar, R. M. Alarming rise in the number and intensity of extreme point rainfall events over the Indian region under climate change scenario. Indian Institute of Tropical Meteorology, 2009.

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11

Tortorelli, Robert L. Depth-duration frequency of precipitation for Oklahoma. U.S. Dept. of the Interior, U.S. Geological Survey, 1999.

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12

Tortorelli, Robert L. Depth-duration frequency of precipitation for Oklahoma. U.S. Dept. of the Interior, U.S. Geological Survey, 1999.

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13

Asquith, William H. Atlas of depth-duration frequency of precipitation annual maxima for Texas. U.S. Dept. of the Interior, U.S. Geological Survey, Water Resources Division, 2004.

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14

Tortorelli, Robert L. Depth-duration frequency of precipitation for Oklahoma. U.S. Dept. of the Interior, U.S. Geological Survey, 1999.

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15

Tortorelli, Robert L. Depth-duration frequency of precipitation for Oklahoma. U.S. Dept. of the Interior, U.S. Geological Survey, 1999.

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16

Tortorelli, Robert L. Depth-duration frequency of precipitation for Oklahoma. U.S. Dept. of the Interior, U.S. Geological Survey, 1999.

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17

Asquith, William H. Atlas of depth-duration frequency of precipitation annual maxima for Texas. U.S. Dept. of the Interior, U.S. Geological Survey, Water Resources Division, 2004.

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18

Asquith, William H. Atlas of depth-duration frequency of precipitation annual maxima for Texas. U.S. Dept. of the Interior, U.S. Geological Survey, Water Resources Division, 2004.

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19

Asquith, William H. Atlas of depth-duration frequency of precipitation annual maxima for Texas. U.S. Dept. of the Interior, U.S. Geological Survey, Water Resources Division, 2004.

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20

Asquith, William H. Depth-duration frequency of precipitation for Texas. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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21

Tortorelli, Robert L. Depth-duration frequency of precipitation for Oklahoma. U.S. Dept. of the Interior, U.S. Geological Survey, 1999.

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22

Tortorelli, Robert L. Depth-duration frequency of precipitation for Oklahoma. U.S. Dept. of the Interior, U.S. Geological Survey, 1999.

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23

Tortorelli, Robert L. Depth-duration frequency of precipitation for Oklahoma. U.S. Dept. of the Interior, U.S. Geological Survey, 1999.

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24

Tortorelli, Robert L. Depth-duration frequency of precipitation for Oklahoma. U.S. Dept. of the Interior, U.S. Geological Survey, 1999.

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25

Asquith, William H. Atlas of depth-duration frequency of precipitation annual maxima for Texas. U.S. Dept. of the Interior, U.S. Geological Survey, Water Resources Division, 2004.

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26

C, Wilson Raymond, Torikai Jill D, Ellen Stephen D, Geological Survey (U.S.), and Honolulu (Hawaii). Dept. of Public Works, eds. Development of rainfall warning thresholds for debris flows in the Honolulu District, Oahu. Dept. of the Interior, U.S. Geological Survey, 1992.

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27

United States. Bureau of Reclamation and Morrison-Knudsen Engineers Inc, eds. Determination of an upper limit design rainstorm for the Colorado River Basin above Hoover Dam. U.S. Dept. of the Interior, Bureau of Reclamation, 1990.

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28

Jet Propulsion Laboratory (U.S.), ed. Shuttle Imaging Radar-B (SIR-B) data analysis for identifying rainfall event occurrence and intensity: Final report. Earth Satellite Corp., 1985.

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29

Lanning-Rush, Jennifer. Extreme precipitation depths for Texas, excluding the Trans-Pecos region. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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30

Lanning-Rush, Jennifer. Extreme precipitation depths for Texas, excluding the Trans-Pecos region. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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31

Lanning-Rush, Jennifer. Extreme precipitation depths for Texas, excluding the Trans-Pecos region. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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32

Lanning-Rush, Jennifer. Extreme precipitation depths for Texas, excluding the Trans-Pecos region. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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33

Rainfall intensity over short periods in Cyprus. The Service, 1985.

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34

Geological Survey (U.S.). Application of methods for analysis of rainfall intensity in areas of Israeli, Jordanian, and Palestinian interest. 2006.

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35

Verification of rain-flow reconstructions of a variable amplitude load history. National Aeronautics and Space Administration, Langley Research Center, 1992.

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36

The Use of Satellite Microwave Rainfall Measurements to Predict Eastern North Pacific Tropical Cyclone Intensity. Storming Media, 1999.

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37

Shuttle Imaging Radar-B (SIR-B) data analysis for identifying rainfall event occurrence and intensity: Final report. Earth Satellite Corp., 1985.

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38

Alarming rise in the number and intensity of extreme point rainfall events over the Indian region under climate change scenario. Indian Institute of Tropical Meteorology, 2009.

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39

Alarming rise in the number and intensity of extreme point rainfall events over the Indian region under climate change scenario. Indian Institute of Tropical Meteorology, 2009.

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40

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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41

Takama, Takeshi, Muhammad Bilal, and K. Srinivasa Raju, eds. Impact of Climate Change on Hydrology and Water Resources. IWA Publishing, 2022. http://dx.doi.org/10.2166/9781789064421.

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Abstract The impact of climate change on water resources is a research area that is gaining prominence, and concerns the prediction of rainfall, temperature, streamflow/discharge, and other meteorological variables. This book is intended to help researchers and other relevant stakeholders working in this area. Its chapters deal with estimation of runoff, floods and droughts, intensity-duration frequency (IDF) curves and evapotranspiration (ET). In addition, some of the miscellaneous topics related to hydrology are also included. In Focus–a book series that showcases the latest accomplishments

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42

Kirch, Patrick V. The Prehistory of Hawai‘i. Edited by Ethan E. Cochrane and Terry L. Hunt. Oxford University Press, 2014. http://dx.doi.org/10.1093/oxfordhb/9780199925070.013.027.

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The Hawaiian Islands are the most isolated inhabited archipelago in the world. Initially colonized around A.D. 1000, the environmental gradients of rainfall and island-age have influenced subsequent cultural variation and differentiation in the islands. Settlements are typically dispersed hamlets and integrated within agricultural facilities such as irrigated pondfields and dryland field systems. Populations were politically organized in idealized pie-shaped units or ahupua`a that typically encompass a cross-section of island resources. Material culture , including fishhooks, stone tools, and

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43

Kaplan, Jonathan, and Federico Paredes Umaña. Water, Cacao, and The Early Maya of Chocóla. University Press of Florida, 2018. http://dx.doi.org/10.5744/florida/9780813056746.001.0001.

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Before the authors’ research, Chocolá was no more than an intriguing legend. Chocolá’s apparent political links to the greatest Preclassic southern Maya area polity, Kaminaljuyu, would make any discovery about Chocolá conceivably vital to a better understanding of Maya origins and New World archaeology, as both ancient cities are located in the Southern Maya Region. Two facts led researchers to search more specifically for the material bases for Chocolá’s rise to power: 1) Mesoamerica’s greatest rainfall, 2) cacao groves around the modern village lying atop the ancient city. Cacao was so impor

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44

Fensholt, Rasmus, Cheikh Mbow, Martin Brandt, and Kjeld Rasmussen. Desertification and Re-Greening of the Sahel. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.553.

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In the past 50 years, human activities and climatic variability have caused major environmental changes in the semi-arid Sahelian zone and desertification/degradation of arable lands is of major concern for livelihoods and food security. In the wake of the Sahel droughts in the early 1970s and 1980s, the UN focused on the problem of desertification by organizing the UN Conference on Desertification (UNCOD) in Nairobi in 1976. This fuelled a significant increase in the often alarmist popular accounts of desertification as well as scientific efforts in providing an understanding of the mechanism

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