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Books on the topic 'Rainfall characteristics'

Author: Grafiati
Published: 4 June 2021
Last updated: 26 January 2023

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1

Sarma, V. V. Jagannadha. Rainfall characteristics of north Andhra. Visakhapatnam: Association of Hydrologists of India, 2003.

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2

Bhatia, K. K. S. Rainfall characteristics in north east India. Roorkee: Western Himalayan Regional Centre, National Institute of Hydrology, 1992.

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3

Huff, Floyd A. 100-year rainstorms in the Midwest: Design characteristics. Champaign, Ill. (2204 Griffith Dr., Champaign 61820-7495): Illinois State Water Survey, 1993.

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4

Liu, An, Ashantha Goonetilleke, and Prasanna Egodawatta. Role of Rainfall and Catchment Characteristics on Urban Stormwater Quality. Singapore: Springer Singapore, 2015. http://dx.doi.org/10.1007/978-981-287-459-7.

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5

Huff, Floyd A. Frequency distribution and hydroclimatic characteristics of heavy rainstorms in Illinois. Champaign, Ill. (2204 Griffith Dr., Champaign 61820): State Water Survey Division, 1988.

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6

Xie, Juying. Satellite-derived rainfall estimates and propagation characteristics associated with mesoscale convective systems (MCSs). Washington, D.C: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Environmental Satellite, Data, and Information Service, 1989.

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7

Xie, Juying. Satellite-derived rainfall estimates and propagation characteristics associated with mesoscale convective systems (MCSs). Washington, D.C: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Environmental Satellite, Data, and Information Service, 1989.

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8

Fleming, Eric L. Characteristics of western region flash flood events in GOES imagery and conventional data. Rockville, MD: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Environmental Satellite, Data, and Information Service, 1986.

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9

Oltmann, R. N. Rainfall and runoff quantity and quality characteristics of four urban land-use catchments in Fresno, California, October 1981 to April 1983. Sacramento, Calif: Dept. of the Interior, U.S. Geological Survey, 1987.

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10

Oltmann, R. N. Rainfall and runoff quantity and quality characteristics of four urban land-use catchments in Fresno, California, October 1981 to April 1983. Washignton: U.S. G.P.O., 1989.

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11

Mustard, Martha H. Runoff characteristics and washoff loads from rainfall-simulation experiments on a street surface and a native pasture in the Denver metropolitan area, Colorado. Washington: U.S. G.P.O., 1987.

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12

Guay, Joel R. Rainfall-runoff characteristics and effects of increased urban density on streamflow and infiltration in the eastern part of the San Jacinto River Basin, Riverside County, California. Sacramento, Calif: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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13

Guay, Joel R. Rainfall-runoff characteristics and effects of increased urban density on streamflow and infiltration in the eastern part of the San Jacinto River Basin, Riverside County, California. Sacramento, Calif: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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14

Guay, Joel R. Rainfall-runoff characteristics and effects of increased urban density on streamflow and infiltration in the eastern part of the San Jacinto River Basin, Riverside County, California. Sacramento, Calif: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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15

Guay, Joel R. Rainfall-runoff characteristics and effects of increased urban density on streamflow and infiltration in the eastern part of the San Jacinto River basin, Riverside County, California. Sacramento, Calif: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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16

Guay, Joel R. Rainfall-runoff characteristics and effects of increased urban density on streamflow and infiltration in the eastern part of the San Jacinto River Basin, Riverside County, California. Sacramento, Calif: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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17

Guay, Joel R. Rainfall-runoff characteristics and effects of increased urban density on streamflow and infiltration in the eastern part of the San Jacinto River Basin, Riverside County, California. Sacramento, Calif: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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18

Guay, Joel R. Rainfall-runoff characteristics and effects of increased urban density on streamflow and infiltration in the eastern part of the San Jacinto River basin, Riverside County, California. Sacramento, Calif: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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19

A, Ranade Ashwini, and Indian Institute of Tropical Meteorology., eds. Characteristics of hydrological wet season over different river basins of India. Pune: Indian Institute of Tropical Meteorology, 2007.

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20

Liu, An, Prasanna Egodawatta, and Ashantha Goonetilleke. Role of Rainfall and Catchment Characteristics on Urban Stormwater Quality. Springer Singapore Pte. Limited, 2015.

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21

Liu, An, Prasanna Egodawatta, and Ashantha Goonetilleke. Role of Rainfall and Catchment Characteristics on Urban Stormwater Quality. Springer Singapore Pte. Limited, 2015.

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22

H, Mustard Martha, and Geological Survey (U.S.), eds. U.S. Geological Survey urban-stormwater data base of constitutent storm loads: Characteristics of rainfall runoff, and antecedent conditions; and basin characteristics. Denver, Colo: Dept. of the Interior, U.S. Geological Survey, 1987.

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23

H, Mustard Martha, and Geological Survey (U.S.), eds. U.S. Geological Survey urban-stormwater data base of constitutent storm loads: Characteristics of rainfall runoff, and antecedent conditions; and basin characteristics. Denver, Colo: Dept. of the Interior, U.S. Geological Survey, 1987.

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24

H, Mustard Martha, and Geological Survey (U.S.), eds. U.S. Geological Survey urban-stormwater data base of constitutent storm loads: Characteristics of rainfall runoff, and antecedent conditions; and basin characteristics. Denver, Colo: Dept. of the Interior, U.S. Geological Survey, 1987.

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25

U.S. Geological Survey urban-stormwater data base of constitutent storm loads: Characteristics of rainfall runoff, and antecedent conditions; and basin characteristics. Denver, Colo: Dept. of the Interior, U.S. Geological Survey, 1987.

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26

H, Mustard Martha, and Geological Survey (U.S.), eds. U.S. Geological Survey urban-stormwater data base of constitutent storm loads: Characteristics of rainfall runoff, and antecedent conditions; and basin characteristics. Denver, Colo: Dept. of the Interior, U.S. Geological Survey, 1987.

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27

U.S. Geological Survey urban-stormwater data base of constitutent storm loads: Characteristics of rainfall runoff, and antecedent conditions; and basin characteristics. Denver, Colo: Dept. of the Interior, U.S. Geological Survey, 1987.

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28

Chan, Johnny C. L. Physical Mechanisms Responsible for Track Changes and Rainfall Distributions Associated with Tropical Cyclone Landfall. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780190676889.013.16.

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As a tropical cyclone approaches land, its interaction with the characteristics of the land (surface roughness, topography, moisture availability, etc.) will lead to changes in its track as well as the rainfall and wind distributions near its landfall location. Accurate predictions of such changes are important in issuing warnings and disaster preparedness. In this chapter, the basic physical mechanisms that cause changes in the track and rainfall distributions when a tropical cyclone is about to make landfall are presented. These mechanisms are derived based on studies from both observations and idealized simulations. While the latter are relatively simple, they can isolate the fundamental and underlying physical processes that are inherent when an interaction between the land and the tropical cyclone circulation takes place. These processes are important in assessing the performance of the forecast models, and hence could help improve the model predictions and subsequently disaster preparedness.
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29

Chan, Johnny C. L. Physical Mechanisms Responsible for Track Changes and Rainfall Distributions Associated with Tropical Cyclone Landfall. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780190699420.013.16.

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As a tropical cyclone approaches land, its interaction with the characteristics of the land (surface roughness, topography, moisture availability, etc.) will lead to changes in its track as well as the rainfall and wind distributions near its landfall location. Accurate predictions of such changes are important in issuing warnings and disaster preparedness. In this chapter, the basic physical mechanisms that cause changes in the track and rainfall distributions when a tropical cyclone is about to make landfall are presented. These mechanisms are derived based on studies from both observations and idealized simulations. While the latter are relatively simple, they can isolate the fundamental and underlying physical processes that are inherent when an interaction between the land and the tropical cyclone circulation takes place. These processes are important in assessing the performance of the forecast models, and hence could help improve the model predictions and subsequently disaster preparedness.
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30

R, Ellis Sherman, Gibbs Johnnie W, Denver Regional Council of Governments, and Geological Survey (U.S.), eds. Runoff characteristics and washoff loads from rainfall-simulation experiments on a street surface and a native pasture in the Denver metropolitan area. Lakewood, Colo: U.S. Dept. of the Interior, Geological Survey, 1985.

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31

Dolman, A. Johannes, Luis U. Vilasa-Abad, and Thomas A. J. Janssen. Ecohydrological Concepts of Water-Vegetation Interaction in the Drylands of Africa. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.554.

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Drylands cover around 40% of the land surface on Earth and are inhabited by more than 2 billion people, who are directly dependent on these lands. Drylands are characterized by a highly variable rainfall regime and inherent vegetation-climate feedbacks that can enhance the resilience of the system, but also can amplify disturbances. In that way, the system may get locked into two alternate stable states: one relatively wet and vegetated, and the other dry and barren. The resilience of dryland ecosystems derives from a number of adaptive mechanisms by which the vegetation copes with prolonged water stress, such as hydraulic redistribution. The stochastic nature of both the vegetation dynamics and the rainfall regime is a key characteristic of these systems and affects its management in relation to the feedbacks. How the ecohydrology of the African drylands will change in the future depends on further changes in climate, human disturbances, land use, and the socioeconomic system.
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32

Entwisle, Timothy. Sprinter and Sprummer. CSIRO Publishing, 2014. http://dx.doi.org/10.1071/9781486302048.

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Since 1788, Australia has carried the yoke of four European seasons that make no sense in most parts of the country. We may like them for historical or cultural reasons, or because they are the same throughout the world, but they tell us nothing of our natural environment. It's time to reject those seasons and to adopt a system that brings us more in tune with our plants and animals – a system that helps us to notice and respond to climate change. Using examples from his 25 years working in botanic gardens, author Timothy Entwisle illustrates how our natural world really responds to seasonal changes in temperature, rainfall and daylight, and why it would be better to divide up the year based on what Australian plants do rather than ancient rites of the Northern Hemisphere. Sprinter and Sprummer opens with the origins and theory of the traditional seasonal system, and goes on to review the Aboriginal seasonal classifications used across Australia. Entwisle then proposes a new five-season approach, explaining the characteristics of each season, along with the biological changes that define them. The book uses seasons to describe the fascinating triggers in the life of a plant (and plant-like creatures), using charismatic flora such as carnivorous plants, the Wollemi Pine and orchids, as well as often overlooked organisms such as fungi. The final chapter considers climate change and how the seasons are shifting whether we like it or not.
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