From 1974 to 1982 repeated tracer tests using fluorescent dyes were carried out in the highly glaciated drainage basin of Vernagtbach. These tests enabled the quantitative determination of the runoff in the forefield of the Vernagtferner, the calculation of travel times of the stream water and estimations of the relative contributions to the entire runoff originating from individual streams. In addition, tracer tests were carried out in the firn area of the glacier resulting in data concerning the storage and travel time of meltwater inside the glacier
Research in 1952-54 on Saskatchewan Glacier was directed toward the measurement of velocity on the s...
Participants Gary Fisher, U.S. Geological Survey (oversees stream flow monitoring) Ed Doheny, U.S. G...
The purpose of this thesis is to investigate the hydrological dynamics of Gornerglestcher and Findel...
This paper describes the extraordinary difficulties met in gauging glacier streams and establishes c...
From 1974 to 1982 repeated tracer tests using fluorescent dyes were carried out in the highly glacia...
[1] In-stream flow protection programs require accurate, real-time streamflow data to aid in the pro...
We first present the results of a series of tracer experiments conducted on an alpine glacier (Gorne...
Participants Gary Fisher, U.S. Geological Survey (oversees stream flow monitoring) Ed Doheny, U.S. G...
Participants Gary Fisher, U.S. Geological Survey (oversees stream flow monitoring) Ed Doheny, U.S. G...
Participants Gary Fisher, U.S. Geological Survey (oversees stream flow monitoring) Ed Doheny, U.S. G...
Participants Gary Fisher, U.S. Geological Survey (oversees stream flow monitoring) Ed Doheny, U.S. G...
Participants Gary Fisher, U.S. Geological Survey (oversees stream flow monitoring) Ed Doheny, U.S. G...
Studies of glacier hydrology rely increasingly on measurements made in boreholes as a basis for reco...
In January/February 1985 a German-South African expedition had the opportunity to repeat measurement...
This study characterizes the glacial and proglacial hydrology of a rapidly deglaciating system at Vi...
Research in 1952-54 on Saskatchewan Glacier was directed toward the measurement of velocity on the s...
Participants Gary Fisher, U.S. Geological Survey (oversees stream flow monitoring) Ed Doheny, U.S. G...
The purpose of this thesis is to investigate the hydrological dynamics of Gornerglestcher and Findel...
This paper describes the extraordinary difficulties met in gauging glacier streams and establishes c...
From 1974 to 1982 repeated tracer tests using fluorescent dyes were carried out in the highly glacia...
[1] In-stream flow protection programs require accurate, real-time streamflow data to aid in the pro...
We first present the results of a series of tracer experiments conducted on an alpine glacier (Gorne...
Participants Gary Fisher, U.S. Geological Survey (oversees stream flow monitoring) Ed Doheny, U.S. G...
Participants Gary Fisher, U.S. Geological Survey (oversees stream flow monitoring) Ed Doheny, U.S. G...
Participants Gary Fisher, U.S. Geological Survey (oversees stream flow monitoring) Ed Doheny, U.S. G...
Participants Gary Fisher, U.S. Geological Survey (oversees stream flow monitoring) Ed Doheny, U.S. G...
Participants Gary Fisher, U.S. Geological Survey (oversees stream flow monitoring) Ed Doheny, U.S. G...
Studies of glacier hydrology rely increasingly on measurements made in boreholes as a basis for reco...
In January/February 1985 a German-South African expedition had the opportunity to repeat measurement...
This study characterizes the glacial and proglacial hydrology of a rapidly deglaciating system at Vi...
Research in 1952-54 on Saskatchewan Glacier was directed toward the measurement of velocity on the s...
Participants Gary Fisher, U.S. Geological Survey (oversees stream flow monitoring) Ed Doheny, U.S. G...
The purpose of this thesis is to investigate the hydrological dynamics of Gornerglestcher and Findel...