JOHN J DRAKE
Datos Biográficos
| ID | 5245176 |
|---|---|
| NOMBRE | JOHN J DRAKE |
| NOMBRES | JOHN J |
| APELLIDO | DRAKE |
| FIRMA | DRAKE J J |
| AFILIACIONES | McMaster University |
| VERIFICADO | No |
| TOTAL DE OBRAS | 4 |
| TOTAL DE CITAS | 2 |
| OBRAS COMO AUTOR | 4 |
| OBRAS COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 1976 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 1987 |
| ÍNDICE H | 1 |
Spatial Analysis of Snow‐and Rain‐Generated Highflows In Southern Ontario
Highflows (including floods) in southern Ontario are often thought to be generated primarily by spring snow‐melt. This paper shows that, on the contrary, a significant proportion of highflows results from rain and rain‐on‐snow. Highflows are divided and analysed according to the generating process. Five parameters are estimated and used to characterize both snowmelt‐ and rainfall‐generated highflows: mean number of events per year; mean date of h…
Modifications of Rain Ph at Scheffervjlle, Quebec
Snow Ph and Dust Loading at Schefferville, Quebec
Problems of acid precipitation in association with industrial activity in areas such as the Great Lakes region are now well‐known (e.g. Hornbeck et al., 1977), and the Canadian Network for Sampling Precipitation (CANSAP) has established monitoring stations across Canada. In communities in northern Canada, however, especially in winter, a considerable amount of SO 2 is liberated locally. It is therefore important to be able to separate local effec…
Solutional Erosion in the Southern Canadian Rockies
Spatial Analysis of Snow‐and Rain‐Generated Highflows In Southern Ontario
Highflows (including floods) in southern Ontario are often thought to be generated primarily by spring snow‐melt. This paper shows that, on the contrary, a significant proportion of highflows results from rain and rain‐on‐snow. Highflows are divided and analysed according to the generating process. Five parameters are estimated and used to characterize both snowmelt‐ and rainfall‐generated highflows: mean number of events per year; mean date of h…
Snow Ph and Dust Loading at Schefferville, Quebec
Problems of acid precipitation in association with industrial activity in areas such as the Great Lakes region are now well‐known (e.g. Hornbeck et al., 1977), and the Canadian Network for Sampling Precipitation (CANSAP) has established monitoring stations across Canada. In communities in northern Canada, however, especially in winter, a considerable amount of SO 2 is liberated locally. It is therefore important to be able to separate local effec…
Solutional Erosion in the Southern Canadian Rockies
Modifications of Rain Ph at Scheffervjlle, Quebec
Snow Ph and Dust Loading at Schefferville, Quebec
Problems of acid precipitation in association with industrial activity in areas such as the Great Lakes region are now well‐known (e.g. Hornbeck et al., 1977), and the Canadian Network for Sampling Precipitation (CANSAP) has established monitoring stations across Canada. In communities in northern Canada, however, especially in winter, a considerable amount of SO 2 is liberated locally. It is therefore important to be able to separate local effec…
Spatial Analysis of Snow‐and Rain‐Generated Highflows In Southern Ontario
Highflows (including floods) in southern Ontario are often thought to be generated primarily by spring snow‐melt. This paper shows that, on the contrary, a significant proportion of highflows results from rain and rain‐on‐snow. Highflows are divided and analysed according to the generating process. Five parameters are estimated and used to characterize both snowmelt‐ and rainfall‐generated highflows: mean number of events per year; mean date of h…
Geography (4 obras) · Cartography (2 obras) · Citation (2 obras) · Computer Science (2 obras) · Geographer (2 obras) · Geology (2 obras) · Geology (2 obras) · History (2 obras) · Hydrology (agriculture) (2 obras) · Library science (2 obras)