Ken Pye
Biographic Data
| ID | 1821552 |
|---|---|
| NAME | Ken Pye |
| GIVEN NAMES | Ken |
| FAMILY NAME | Pye |
| SIGNATURE | PYE K |
| AFFILIATIONS | Royal Holloway University of London |
| ORCID | 0000-0002-0075-4342 |
| VERIFIED | Yes |
| TOTAL WORKS | 8 |
| TOTAL CITATIONS | 10 |
| WORKS AS AUTHOR | 8 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1985 |
| LATEST PUBLICATION YEAR | 2003 |
| H-INDEX | 2 |
The use of historical bathymetric charts in a GIS to assess morphological change in estuaries
Navigational charts are a valuable data source for the study of morphological change in estuaries, as they provide bathymetric information of many estuaries, and span a vast period of time. Charts are suitable for studying patterns of morphological change, such as shoal and channel migration. In addition, sequential bathymetric charts or bed surveys can be used to calculate sedimentation and erosion rates. However, a number of problems arise when…
Gradistat
Grain size analysis is an essential tool for classifying sedimentary environments. The calculation of statistics for many samples can, however, be a laborious process. A computer program called GRADISTAT has been written for the rapid analysis of grain size statistics from any of the standard measuring techniques, such as sieving and laser granulometry. Mean, mode, sorting, skewness and other statistics are calculated arithmetically and geometric…
A revised chronology for aeolian activity in subarctic Fennoscandia during the Holocene
Detailed sedimentological studies and parallel sampling for 14 C and infra-red stimulated luminescence age assays were undertaken at six sites lying beyond and below the tree-line with the objective of establishing the historical development of aeolian landforms in Lapland. The main issues were: (a) the timing of dune activity and processes of stabilization; (b) the specific processes responsible for the past and contemporary activity. New data i…
Aeolian Geomorphology
Environmental Change in Drylands
The nature, origin and accumulation of loess
Environmental Change in Drylands Biogeographical and Geomorphological Perspectives
An Introduction to the Physical Geography of the Kora Area, Central Kenya
Environmental Change in Drylands Biogeographical and Geomorphological Perspectives
The use of historical bathymetric charts in a GIS to assess morphological change in estuaries
Navigational charts are a valuable data source for the study of morphological change in estuaries, as they provide bathymetric information of many estuaries, and span a vast period of time. Charts are suitable for studying patterns of morphological change, such as shoal and channel migration. In addition, sequential bathymetric charts or bed surveys can be used to calculate sedimentation and erosion rates. However, a number of problems arise when…
A revised chronology for aeolian activity in subarctic Fennoscandia during the Holocene
Detailed sedimentological studies and parallel sampling for 14 C and infra-red stimulated luminescence age assays were undertaken at six sites lying beyond and below the tree-line with the objective of establishing the historical development of aeolian landforms in Lapland. The main issues were: (a) the timing of dune activity and processes of stabilization; (b) the specific processes responsible for the past and contemporary activity. New data i…
Environmental Change in Drylands
An Introduction to the Physical Geography of the Kora Area, Central Kenya
An Introduction to the Physical Geography of the Kora Area, Central Kenya
The nature, origin and accumulation of loess
Environmental Change in Drylands Biogeographical and Geomorphological Perspectives
Environmental Change in Drylands
Aeolian Geomorphology
A revised chronology for aeolian activity in subarctic Fennoscandia during the Holocene
Detailed sedimentological studies and parallel sampling for 14 C and infra-red stimulated luminescence age assays were undertaken at six sites lying beyond and below the tree-line with the objective of establishing the historical development of aeolian landforms in Lapland. The main issues were: (a) the timing of dune activity and processes of stabilization; (b) the specific processes responsible for the past and contemporary activity. New data i…
Gradistat
Grain size analysis is an essential tool for classifying sedimentary environments. The calculation of statistics for many samples can, however, be a laborious process. A computer program called GRADISTAT has been written for the rapid analysis of grain size statistics from any of the standard measuring techniques, such as sieving and laser granulometry. Mean, mode, sorting, skewness and other statistics are calculated arithmetically and geometric…
The use of historical bathymetric charts in a GIS to assess morphological change in estuaries
Navigational charts are a valuable data source for the study of morphological change in estuaries, as they provide bathymetric information of many estuaries, and span a vast period of time. Charts are suitable for studying patterns of morphological change, such as shoal and channel migration. In addition, sequential bathymetric charts or bed surveys can be used to calculate sedimentation and erosion rates. However, a number of problems arise when…
Geology (6 works) · Geography (5 works) · Geology (5 works) · Physical geography (5 works) · Oceanography (4 works) · Aeolian processes (3 works) · Aeolian processes and effects (3 works) · Climate change (3 works) · Geology and Paleoclimatology Research (3 works) · Geomorphology (3 works)