Skip to main content

Abstract

Hydrology’s history is rooted in early civilizations when humanity began to manage water in their transformation from a nomadic existence to an agrarian society. The development of civilization as we know it has been directly related to humanity’s success in managing the rivers and developing ground water. However, hydrology did not develop as a scientific discipline until measurements, theories, and design equations were developed.

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 36.00
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

Preview

Unable to display preview. Download preview PDF.

Unable to display preview. Download preview PDF.

References

  • Biswas, A.K., 1972: A History of Hydrology. 2d ed. North-Holland Publishing, 336 pp.

    Google Scholar 

  • Chahine, M.T., 1992: The hydrologic cycle and its influence on climate. Nature, 359, 373–380.

    Article  Google Scholar 

  • Chow, V.T., Ed., 1964: Handbook of Applied Hydrology. McGraw-Hill.

    Google Scholar 

  • Dozier, J., 1992: Opportunities to improve hydrologic data. Rev. Geophys., 30 (4), 315–331.

    Article  Google Scholar 

  • Federal Council for Science and Technology, 1962: Scientific Hydrology. U.S. Government Printing Office, 37 pp.

    Google Scholar 

  • Grayson, R.B., I.D. Moore, and T.A. McMahon, 1992a: Physically based hydrologic modeling. 1. A terrain-based model for investigative purposes. Water Resour. Res. 28, 2639–2658.

    Article  Google Scholar 

  • Grayson, R.B., I.D. Moore, and T.A. McMahon, 1992b: Physically based hydrologic modeling. 2. Is the concept realistic? Water Resour. Res. 28, 2659–2666.

    Article  Google Scholar 

  • Gumbel, E.J., 1941: The return period of flood flows. Ann. Math. Stat., 12, 163–190.

    Article  Google Scholar 

  • Hazen, A., 1930: Flood Flows, a Study of Frequencies and Magnitudes. John Wiley & Sons, 199 pp.

    Google Scholar 

  • Hornberger, G.M., 1992: Hydrologic science: Keeping pace with changing values and perceptions. Proc. 10th Symp. on Sustaining Our Water Resources, National Academy Press, 43–58.

    Google Scholar 

  • Hornberger, G.M., 1994: Data and analysis note: A new type of article for water resources research. Water Resour. Res., 30, 3241–3242.

    Article  Google Scholar 

  • Horton, R.E., 1933: The role of infiltration in the hydrologic cycle. Trans. Amer. Geophys. Union, 14, 446–460.

    Article  Google Scholar 

  • Jackson, T.J., D.M. LeVine, C.T. Swift, T.J. Schmugge, and F.R. Schiebe, 1995: Large area mapping of soil moisture using the ESTAR passive microwave radiometer in Washita ’82. Remote Sens. Environ., 53, 27–37.

    Article  Google Scholar 

  • Jakeman, A.J., and G.M. Hornberger, 1993: How much complexity is warranted in a rainfall—runoff model? Water Resour. Res., 29, 2637–2649.

    Article  Google Scholar 

  • Kalinin, G.P., and P.I. Miljukov, 1957: On the computation of unsteady flow in open channels. Meterol. Gidrol. Z., 10, 10–80.

    Google Scholar 

  • Leopold, L.B., and K.S. Davis, 1966: Water. Time Incorporated, 200 pp.

    Google Scholar 

  • Loague, K.M., and R.A. Freeze, 1985: A comparison of rainfall—runoff-modeling techniques on small upland catchments. Water Resour. Res., 21, 229–248.

    Article  Google Scholar 

  • Maidment, D.R., Ed., 1993: Hydrology. Handbook of Hydrology, McGraw-Hill, 1.1–1.15.

    Google Scholar 

  • Martinec, J., 1960: The degree day factor for snowmelt runoff forecasting. Surface Waters, International Union Geodesy Geophys. Gen. Assembly of Helsinki, International Assoc. Hydrol. Sci. Comm., IAHS Publ. 51, 468–477.

    Google Scholar 

  • McCuen, R.H., and W.J. Rawls, 1979: Classification of evaluation of flood flow frequency estimation techniques. Water Res. Bull., 15, 88–93.

    Article  Google Scholar 

  • Nace, R.L., 1974: General evolution of the concept of the hydrologic cycle. Three Centuries of Scientific Hydrology, UNESCO, WMO, IAHS, 40–44.

    Google Scholar 

  • Naef, F., 1981: Can we model the rainfall–runoff process today? Hydrologic Sci. Bull., 26, 281–289.

    Article  Google Scholar 

  • NRC, 1991: Opportunities in the Hydrologic Sciences. National Academy Press, 348 pp.

    Google Scholar 

  • Philip, J.R., 1957: The theory of infiltration: 1. The infiltration equation and its solution. Soil Sci., 83, 345–357.

    Article  Google Scholar 

  • Sherman, L.K., 1932: Stream flow from rainfall by the unit-graph method. Eng. News. Rec., 108, 501–505.

    Google Scholar 

  • Theis, C.V., 1935: The relation between lowering of the piezometric surface and the rate and duration of discharge of a well using groundwater storage. Trans. Amer. Geophys. Union, 16th Annual Meeting, 519–524.

    Google Scholar 

  • Water Resources Council, 1981: Estimating Peak Flow Frequencies for Natural Ungaged Watersheds—A Proposed Nationwide Test. U.S. Water Resources Council Hydrology Committee, 346 pp.

    Google Scholar 

Download references

Authors

Editor information

James Rodger Fleming

Rights and permissions

Reprints and permissions

Copyright information

© 1996 American Meteorological Society

About this chapter

Cite this chapter

Engman, E.T. (1996). Hydrology in the Twentieth Century. In: Fleming, J.R. (eds) Historical Essays on Meteorology 1919–1995. American Meteorological Society, Boston, MA. https://doi.org/10.1007/978-1-940033-84-6_14

Download citation

  • DOI: https://doi.org/10.1007/978-1-940033-84-6_14

  • Publisher Name: American Meteorological Society, Boston, MA

  • Online ISBN: 978-1-940033-84-6

  • eBook Packages: Springer Book Archive

Publish with us

Policies and ethics