SPRI library catalogue
View a record
Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.
Please search for material in iDiscover for up-to-date information about the library collection.
Record #112838:
Global change: can we detect its effect on subalpine hydrographs? / Charles A. Troendle.
Title: | Global change: can we detect its effect on subalpine hydrographs? / Charles A. Troendle. |
Author(s): | Troendle, Charles A. |
Date: | 1991. |
In: | Western Snow Conference. Proceedings. (1991.), Vol. 59th Annual Meeting (1991) |
Abstract: | Subalpine water balance model was used to simulate effect of temperature and precipitation change on streamflow from subalpine forests. Comparisons are made between simulated change and long-term variability of observed flow. Magnitude of simulated flows was well within range of observed flow, but timing of peak, under warming scenario, was advanced three weeks. |
Notes: | Western Snow Conference. Proceedings. Vol. 59th Annual Meeting :1-8 (1991). |
Keywords: | 551.58 -- Climatology. 551.583 -- Climatic changes. 551.588.5 -- Climate, relationship with ice. 551.579 -- Hydrometeorology. 551.579.3 -- Water supply from glaciers. 556 -- Hydrology. E11 -- Glaciology: glaciohydrology. |
SPRI record no.: | 112838 |
LDR 01300naa#a2200000#a#4500 001 SPRI-112838 005 20230329175540.0 007 ta 008 230329s1991####xx####|##|###|0||#0|eng#d 035 ## ‡aSPRI-112838 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aTroendle, Charles A. 245 10 ‡aGlobal change :‡bcan we detect its effect on subalpine hydrographs? /‡cCharles A. Troendle. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 1-8. 500 ## ‡aWestern Snow Conference. Proceedings. Vol. 59th Annual Meeting :1-8 (1991). 520 3# ‡aSubalpine water balance model was used to simulate effect of temperature and precipitation change on streamflow from subalpine forests. Comparisons are made between simulated change and long-term variability of observed flow. Magnitude of simulated flows was well within range of observed flow, but timing of peak, under warming scenario, was advanced three weeks. 650 07 ‡a551.58 -- Climatology.‡2udc 650 07 ‡a551.583 -- Climatic changes.‡2udc 650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc 650 07 ‡a551.579 -- Hydrometeorology.‡2udc 650 07 ‡a551.579.3 -- Water supply from glaciers.‡2udc 650 07 ‡a556 -- Hydrology.‡2udc 650 07 ‡aE11 -- Glaciology: glaciohydrology.‡2local 773 0# ‡7nnas ‡tWestern Snow Conference. Proceedings. ‡gVol. 59th Annual Meeting (1991) ‡wSPRI-26976 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230329