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Record #88901:
- #88901
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MARC recordDistribution of snow cover as influenced by landscape units in southwestern Ontario / H.O. Schroeter, H.R. Whiteley.
| Title: | Distribution of snow cover as influenced by landscape units in southwestern Ontario / H.O. Schroeter, H.R. Whiteley. |
| Author(s): | Schroeter, H. O. Whiteley, H. R. |
| Date: | 1987. |
| In: | Eastern Snow Conference. Proceedings. (1987.), Vol. 43rd [1986] Annual Meeting (1987) |
| Abstract: | Snow-depth distribution patterns in upper Grand River watershed for winter 1985-86 are given for different land-cover types, as well as for edges (e.g. fence lines). Representative snow densities are presented for each cover type and edge effect. Temporal changes in distribution pattern show that, at maximum accumulation, open fields contain less snow than average, and edges and ditches more than average. After sustained ablation, almost all snow is in edges and ditches. From comparison of estimates of snow water equivalents, it was shown that estimates of mean basin water equivalent need to account for not only different land-cover types, but also for edge effects. |
| Notes: | Eastern Snow Conference. Proceedings. Vol. 43rd [1986] Annual Meeting :32-44 (1987). |
| Keywords: | 551.578.42 -- Snow surveys. 556 -- Hydrology. 551.579.2 -- Water supply from snow. E10 -- Glaciology: snow and avalanches. |
| SPRI record no.: | 88901 |
LDR 01563naa#a2200000#a#4500 001 SPRI-88901 005 20230321022645.0 007 ta 008 230321s1987####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-88901 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aSchroeter, H. O. 245 10 ‡aDistribution of snow cover as influenced by landscape units in southwestern Ontario /‡cH.O. Schroeter, H.R. Whiteley. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1987. 300 ## ‡ap. 32-44 :‡bill., diags., tables, maps. 500 ## ‡aEastern Snow Conference. Proceedings. Vol. 43rd [1986] Annual Meeting :32-44 (1987). 520 3# ‡aSnow-depth distribution patterns in upper Grand River watershed for winter 1985-86 are given for different land-cover types, as well as for edges (e.g. fence lines). Representative snow densities are presented for each cover type and edge effect. Temporal changes in distribution pattern show that, at maximum accumulation, open fields contain less snow than average, and edges and ditches more than average. After sustained ablation, almost all snow is in edges and ditches. From comparison of estimates of snow water equivalents, it was shown that estimates of mean basin water equivalent need to account for not only different land-cover types, but also for edge effects. 650 07 ‡a551.578.42 -- Snow surveys.‡2udc 650 07 ‡a556 -- Hydrology.‡2udc 650 07 ‡a551.579.2 -- Water supply from snow.‡2udc 650 07 ‡aE10 -- Glaciology: snow and avalanches.‡2local 700 1# ‡aWhiteley, H. R. 773 0# ‡7nnas ‡tEastern Snow Conference. Proceedings. ‡gVol. 43rd [1986] Annual Meeting (1987) ‡wSPRI-23848 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230321