๐”– Bobbio Scriptorium
โœฆ   LIBER   โœฆ

Morphometric controls and geomorphic responses on fans in the Southern Alps, New Zealand

โœ Scribed by Fes A. de Scally; Ian F. Owens


Publisher
John Wiley and Sons
Year
2004
Tongue
English
Weight
368 KB
Volume
29
Category
Article
ISSN
0360-1269

No coin nor oath required. For personal study only.


๐Ÿ“œ SIMILAR VOLUMES


Controls on spatial variability in snow
โœ Heather Purdie; Brian Anderson; Wendy Lawson; Andrew Mackintosh ๐Ÿ“‚ Article ๐Ÿ“… 2010 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 418 KB

## Abstract Net accumulation measurements from two glaciers located on opposite sides of the New Zealand Southern Alps were used to explore processes controlling spatial variability. The degree of variability, as measured by the spatial variogram, differed in each of the three successive years, but

Energy balance and synoptic climatology
โœ Neale, S. M.; Fitzharris, B. B. ๐Ÿ“‚ Article ๐Ÿ“… 1997 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 458 KB ๐Ÿ‘ 2 views

Snow melt is calculated at 1780 m a.s.l., near the Main Divide of the Southern Alps, using a bulk aerodynamic energy balance approach. Results are related to melt measured directly using a lysimeter and to synoptic weather patterns. Measurements are taken half hourly, over a 38 day period from the s

Interannual variation in end-of-summer s
โœ G. R. Clare; B.B. Fitzharris; T. J. H. Chinn; M. J. Salinger ๐Ÿ“‚ Article ๐Ÿ“… 2002 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 387 KB

The end-of-summer snowline (EOSS) on 47 glaciers distributed throughout the Southern Alps of New Zealand is related to changes in Southern Hemisphere atmospheric circulation and sea surface temperature patterns over a 23 year period. The EOSS provides an index of the glacier mass balance, as high (

The Pleistocene Cape Kidnappers section
โœ Jean-Noรซl Proust; Frank Chanier ๐Ÿ“‚ Article ๐Ÿ“… 2004 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 492 KB

## Abstract High sedimentation rates in Pleistocene active margin basins can provide a very detailed record of tectonic and climatic controls on sediment preservation. A 500โ€‰m thick, Pleistocene rock section exposed in northeastern North Island of New Zealand (Kidnappers Group), provides the opport