Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Harold C. Troxell"'
Autor:
Harold C. Troxell, W. G. Hoyt
Publikováno v:
Transactions of the American Society of Civil Engineers. 99:1-30
The effect on stream flow of changes in forest and brush cover on specifio natural areas is described in this paper. An experiment by the United State Forest Service and the United States Weather B...
Autor:
Harold C. Troxell, R. Stanley Lord, Franklin Thomas, Ivan E. Houk, Donald M. Baker, A. L. Sonderegger, R. W. Davenport, F. C. Finkle, James M. Fox, Gordon R. Williams, Karl J. Bermel, Walter J. Wood, Maxwell F. Burke
Publikováno v:
Transactions of the American Society of Civil Engineers. 106:219-263
Autor:
W. G. Hoyt, Harold C. Troxell
Publikováno v:
Transactions of the American Society of Civil Engineers. 99:94-111
Publikováno v:
Transactions of the American Society of Civil Engineers. 94:1269-1303
Autor:
Harold C. Troxell, C.E. Burgess
Publikováno v:
Open-File Report.
Autor:
Harold C. Troxell
Although favored with many desirable climatic features, the arid and semiarid valleys of southern California have experienced recurring dry periods throughout the ages. Records of tree-ring growth in the mountain areas for the last 560 years show tha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::77aab73ac95bbe3324711677031dd733
https://doi.org/10.3133/wsp1366
https://doi.org/10.3133/wsp1366
Autor:
Harold C. Troxell, Harry Dennis Wilson
Publikováno v:
Open-File Report.
Autor:
Harold C. Troxell, Harlowe M. Stafford
Publikováno v:
Transactions, American Geophysical Union. 25:21
In interpretation and use of basic hydrological data as basis for planning any public works for conservation or control of water, there is great need for a careful and thorough analysis of the precipitation-runoff relations. Moreover, when such relat
Autor:
Harold C. Troxell
Publikováno v:
Transactions, American Geophysical Union. 34:552
The steep and rugged mountains of Southern California contain considerable ground-water storage. A large portion of the runoff is seepage from this storage The variations in runoff distribution depend on the geology, physiography, and soil cover of t