R A Bagnold

Biographic Data

ID3752108
NAMER A Bagnold
GIVEN NAMESR A
FAMILY NAMEBagnold
SIGNATUREBAGNOLD R A
VERIFIEDNo
TOTAL WORKS23
TOTAL CITATIONS79
AUTHOR COUNT23
EDITOR COUNT0
FIRST PUBLICATION YEAR1931
LATEST PUBLICATION YEAR1992
H-INDEX5

  • Sand Wind and War

    Colin R Thorne, R A BagnoldARTICLEGeographical Journal1992

  • Sand Formations in Southern Arabia

    R A BagnoldARTICLEGeographical Journal1951Cited by: 1

  • Saharan Sand Dunes and the Origin of the Longitudinal Dune

    Open AccessW Armstrong Price, Robert Capot-Rey et al.ARTICLEGeographical Review1950

  • Desert Borderlands of Oman

    Harry Lindsay, Abdul Rahman Halaissie et al.ARTICLEGeographical Journal1950

    Before the paper the President (Sir Harry Lindsay) said: Mr. Thesiger is so well known to us that there is little I need say by way of introduction except that he is continuing his travels in Arabia. His journey on this occasion has been in central Oman, an area he has been the first Englishman to penetrate during the past fifty or so years. His detailed mapping of unexplored country is especially valuable in view of the changes which are likely …

  • Early Days of the Long Range Desert Group

    R A BagnoldARTICLEGeographical Journal1945Cited by: 1

  • The Physics of Blown Sand and Desert Dunes

    Open AccessH T U Smith, R A BagnoldARTICLEGeographical Review1943Cited by: 5

  • The Physics of Blown Sand and Desert Dunes

    Hui Kho J, R A BagnoldARTICLEGeographical Journal1941Cited by: 13

  • The Road to Chephren's Quarries

    Philip Chetwode, Oliver H Myers et al.ARTICLEGeographical Journal1939

    the name of a scribe Para'emhab (read by M. Czerny), the other was illegible. Last year we were obliged to head for home on February 14 and had an uneventful run to near the Dam. Before dawn Engelbach left to catch the aeroplane back to Cairo. He had had a busy week. Fate reserved for us one more surprise: our beginners' luck held good to the end. We left at half-past nine for Idfu and Luxor, and 4 miles from camp, while crossing the AswanKurkur …

  • An Expedition to the Gilf Kebir and 'Uweinat, 1938

    R A Bagnold, Oliver H Myers et al.ARTICLEGeographical Journal1939Cited by: 22

  • The Southern Lut and Iranian Baluchistan

    Charles Close, Percy Sykes et al.ARTICLEGeographical Journal1938

  • The Last of the Zerzura Legend

    R A Bagnold, L E de AlmasyARTICLEGeographical Journal1937Cited by: 2

  • The Culbin Sands and Burghead Bay

    Henry Balfour, R A Bagnold et al.ARTICLEGeographical Journal1937Cited by: 1

  • The Transport of Sand by Wind

    R A BagnoldARTICLEGeographical Journal1937Cited by: 4

    The subject of course is but a special case of the general problem of the transport of solid particles by fluids. The Reynolds' Numbers involved are of the same order, whether sand is transported by air or water, and the type of motion of the grains, and their resulting drag on the fluid, appear to be much the same, though too close a parallel should not be drawn since the density ratios of sand and fluid differ greatly in the two cases. But beca…

  • An Expedition in the Southern Libyan Desert

    Percy Cox, Michael H Mason et al.ARTICLEGeographical Journal1936

  • The Libyan Desert

    R A BagnoldARTICLEAfrican Affairs1936Cited by: 3

    Journal Article THE LIBYAN DESERT Get access R. A. BAGNOLD R. A. BAGNOLD Search for other works by this author on: Oxford Academic Google Scholar African Affairs, Volume XXXV, Issue CXL, July 1936, Pages 294–305, https://doi.org/10.1093/oxfordjournals.afraf.a101512 Published: 01 July 1936

  • Libyan Sands

    R A BagnoldBOOKLibyan Sands1935

  • The Movement of Desert Sand

    Percy Cox, K S Sandford et al.ARTICLEGeographical Journal1935

  • Explorations Sahariennes

    Percy Cox, Francis Rodd et al.ARTICLEGeographical Journal1935

  • The Movement of Desert Sand

    R A BagnoldARTICLEGeographical Journal1935Cited by: 4

    It is well known that on a dry sand beach and, on a much larger scale, on sand-strewn desert country the wind, if above a certain strength, will cause the surface sand grains to rise and to travel down-wind as a low-flying cloud. The mechanism, however, by which ( a ) the grains composing this cloud are raised, ( b ) the rate of mass movement of the sand depends upon the wind velocity, or ( c ) the wind velocity close to the surface is affected b…

  • A Further Journey Through the Libyan Desert

    R A BagnoldARTICLEGeographical Journal1933Cited by: 10

  • A Further Journey Through the Libyan Desert (Continued)

    R A Bagnold, K S Sandford et al.ARTICLEGeographical Journal1933Cited by: 3

    R. A. Bagnold, K. S. Sandford, W. B. K. Shaw, R. E. Moreau, N. D. Riley, T. Hutchinson, V. F. Craig, A Further Journey Through the Libyan Desert (Continued), The Geographical Journal, Vol. 82, No. 3 (Sep., 1933), pp. 211-235

  • Journeys in the Libyan Desert 1929 and 1930

    D Newbold, R A Bagnold et al.ARTICLEGeographical Journal1931

  • Journeys in the Libyan Desert 1929 and 1930

    R A BagnoldARTICLEGeographical Journal1931Cited by: 10