R A Bagnold
Datos Biográficos
| ID | 3752108 |
|---|---|
| NOMBRE | R A Bagnold |
| NOMBRES | R A |
| APELLIDO | Bagnold |
| FIRMA | BAGNOLD R A |
| VERIFICADO | No |
| TOTAL DE OBRAS | 23 |
| TOTAL DE CITAS | 79 |
| TOTAL COMO AUTOR | 23 |
| TOTAL COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 1931 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 1992 |
| ÍNDICE H | 5 |
Sand Wind and War
Sand Formations in Southern Arabia
Saharan Sand Dunes and the Origin of the Longitudinal Dune
Desert Borderlands of Oman
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
The Physics of Blown Sand and Desert Dunes
The Physics of Blown Sand and Desert Dunes
The Road to Chephren's Quarries
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
The Southern Lut and Iranian Baluchistan
The Last of the Zerzura Legend
The Culbin Sands and Burghead Bay
The Transport of Sand by Wind
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
The Libyan Desert
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
The Movement of Desert Sand
Explorations Sahariennes
The Movement of Desert Sand
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
A Further Journey Through the Libyan Desert (Continued)
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
Journeys in the Libyan Desert 1929 and 1930
An Expedition to the Gilf Kebir and 'Uweinat, 1938
The Physics of Blown Sand and Desert Dunes
A Further Journey Through the Libyan Desert
Journeys in the Libyan Desert 1929 and 1930
The Physics of Blown Sand and Desert Dunes
The Transport of Sand by Wind
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…
The Movement of Desert Sand
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…
The Libyan Desert
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
A Further Journey Through the Libyan Desert (Continued)
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
The Last of the Zerzura Legend
Sand Formations in Southern Arabia
Early Days of the Long Range Desert Group
The Culbin Sands and Burghead Bay
Journeys in the Libyan Desert 1929 and 1930
Journeys in the Libyan Desert 1929 and 1930
A Further Journey Through the Libyan Desert
A Further Journey Through the Libyan Desert (Continued)
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
Libyan Sands
The Movement of Desert Sand
Explorations Sahariennes
The Movement of Desert Sand
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…
An Expedition in the Southern Libyan Desert
The Libyan Desert
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
The Last of the Zerzura Legend
The Culbin Sands and Burghead Bay
The Transport of Sand by Wind
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…
The Southern Lut and Iranian Baluchistan
The Road to Chephren's Quarries
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
The Physics of Blown Sand and Desert Dunes
The Physics of Blown Sand and Desert Dunes
Early Days of the Long Range Desert Group
Saharan Sand Dunes and the Origin of the Longitudinal Dune
Desert Borderlands of Oman
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 …
Sand Formations in Southern Arabia
Sand Wind and War
Geography (21 obras) · Geology (17 obras) · Geology (16 obras) · Desert (philosophy (11 obras) · Political science (10 obras) · Law (8 obras) · Aeolian processes and effects (7 obras) · Law (7 obras) · Physical geography (7 obras) · Archaeology (6 obras)