𝔖 Bobbio Scriptorium
✦   LIBER   ✦

Sublimation from snow surface in southern mountain taiga of eastern Siberia

✍ Scribed by Zhang, Yiensheng

Book ID
119661552
Publisher
American Geophysical Union
Year
2004
Tongue
English
Weight
495 KB
Volume
109
Category
Article
ISSN
0148-0227

No coin nor oath required. For personal study only.

πŸ“œ SIMILAR VOLUMES

Moss beneath a leafless larch canopy: in
Moss beneath a leafless larch canopy: influence on water and energy balances in the southern mountainous taiga of eastern Siberia
✍ Kazuyoshi Suzuki; Jumpei Kubota; Hironori Yabuki; Tetsuo Ohata; Valery Vuglinsky πŸ“‚ Article πŸ“… 2007 πŸ› John Wiley and Sons 🌐 English βš– 811 KB

## Abstract The southern mountainous taiga of eastern Siberia has a sparse larch canopy and an understory dominated by a thick moss layer. The physiology of moss is very different from that of other plants, as mosses lack roots and vascular systems and take up water directly. During May 2002, we co

Hydrometeorological effects of intercept
Hydrometeorological effects of intercepted snow in an eastern Siberian taiga forest using a land-surface model
✍ Takeshi Yamazaki; Hironori Yabuki; Tetsuo Ohata πŸ“‚ Article πŸ“… 2007 πŸ› John Wiley and Sons 🌐 English βš– 241 KB πŸ‘ 1 views

## Abstract This study investigates the hydrometeorological effects of intercepted snow in an intensely cold region. Observation of meteorological and hydrological elements in severely cold conditions, such as those in Siberia, is very difficult. One such typical element is that of snow interceptio

Seasonal changes in runoff characteristi
Seasonal changes in runoff characteristics on a permafrost watershed in the southern mountainous region of eastern Siberia
✍ Yusuke Yamazaki; Jumpei Kubota; Tetsuo Ohata; Varely Vuglinsky; Takahisa Mizuyam πŸ“‚ Article πŸ“… 2006 πŸ› John Wiley and Sons 🌐 English βš– 611 KB

## Abstract We attempted to clarify the runoff characteristics of a permafrost watershed in the southern mountainous region of eastern Siberia using hydrological and meteorological data obtained by the State Hydrological Institute in Russia from 1976 to 1985. We analysed seasonal changes in the dir