Scott Polar Research InstituteSPRI library catalogue
Search the catalogue
Browse recordsView 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 It is no longer being updated, so does not reliably reflect our current library holdings.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 #94193:
- #94193
Main publication details
MARC recordStreamflow characteristics of the Qinghai (northern Tibetan) plateau / Zhengniang Yang, Ming-ko Woo.
| Title: | Streamflow characteristics of the Qinghai (northern Tibetan) plateau / Zhengniang Yang, Ming-ko Woo. |
| Author(s): | Yang, Zhengniang. Woo, Ming-ko. |
| Date: | 1988. |
| Publisher: | Trondheim: Tapir Publishers |
| In: | Permafrost. Fifth International Conference. August 2-5, 1988. Proceedings. (1988.), Vol. 1. |
| Abstract: | Permafrost occurs above 4200 m. Three types of runoff patterns may be distinguished according to primary sources of water: snowmelt and rainfall, glacier melt and snowmelt, and groundwater. Large rivers generally drain more than one environment and runoff regime reflects integration of various flow patterns found on plateau. |
| Notes: | In: Permafrost. Fifth International Conference. August 2-5, 1988. Proceedings. Vol. 1. / Kaare Senneset, ed. |
| Keywords: | 556 -- Hydrology. 551.579 -- Hydrometeorology. 551.579.2 -- Water supply from snow. 551.579.3 -- Water supply from glaciers. 556.324 -- Groundwater. E11 -- Glaciology: glaciohydrology. (510) -- People's Republic of China. |
| SPRI record no.: | 94193 |
LDR 01430naa#a2200000#a#4500 001 SPRI-94193 005 20240416160718.0 007 ta 008 240416s1988####no#ab##|#####|0||#0#eng#d 035 ## ‡aSPRI-94193 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aYang, Zhengniang. 245 10 ‡aStreamflow characteristics of the Qinghai (northern Tibetan) plateau /‡cZhengniang Yang, Ming-ko Woo. 260 ## ‡aTrondheim :‡bTapir Publishers,‡c1988. 300 ## ‡ap. 650-655 :‡bdiags., maps. 500 ## ‡aIn: Permafrost. Fifth International Conference. August 2-5, 1988. Proceedings. Vol. 1. / Kaare Senneset, ed. 520 3# ‡aPermafrost occurs above 4200 m. Three types of runoff patterns may be distinguished according to primary sources of water: snowmelt and rainfall, glacier melt and snowmelt, and groundwater. Large rivers generally drain more than one environment and runoff regime reflects integration of various flow patterns found on plateau. 650 07 ‡a556 -- Hydrology.‡2udc 650 07 ‡a551.579 -- Hydrometeorology.‡2udc 650 07 ‡a551.579.2 -- Water supply from snow.‡2udc 650 07 ‡a551.579.3 -- Water supply from glaciers.‡2udc 650 07 ‡a556.324 -- Groundwater.‡2udc 650 07 ‡aE11 -- Glaciology: glaciohydrology.‡2local 651 #7 ‡a(510) -- People's Republic of China.‡2udc 700 1# ‡aWoo, Ming-ko. 773 0# ‡7nnam ‡aKaare Senneset, ed. ‡tPermafrost. Fifth International Conference. August 2-5, 1988. Proceedings. ‡dTrondheim : Tapir Publishers, 1988. ‡gVol. 1. ‡wSPRI-93838 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240416