Saved in:
Bibliographic Details
Main Authors: Irvine-Fynn, Tristram D L, Porter, P R, Rowan, Ann V, Quincey, Duncan J, Gibson, Morgan J, Bridge, J W, Watson, C Scott, Hubbard, Alun L, Glasser, Neil F
Format: Dataset Open Access
Language:en
Published: PANGAEA 2017
Subjects:
Online Access:https://doi.org/10.1594/PANGAEA.883419
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1867171003219574784
author Irvine-Fynn, Tristram D L
Porter, P R
Rowan, Ann V
Quincey, Duncan J
Gibson, Morgan J
Bridge, J W
Watson, C Scott
Hubbard, Alun L
Glasser, Neil F
author_facet Irvine-Fynn, Tristram D L
Porter, P R
Rowan, Ann V
Quincey, Duncan J
Gibson, Morgan J
Bridge, J W
Watson, C Scott
Hubbard, Alun L
Glasser, Neil F
collection Datos científicos de ciencias marinas y ambientales
contents A hydrological monitoring station for Khumbu Glacier, Nepal, was established in a stable reach of the sole outflow channel at 4930 m a.s.l.. at approximately 27°56'02"N 86°48'44"E where meltwater breaches the lateral/terminal moraine ridge. Average water stage (S) was recorded at 30 min intervals using a Druck PDCR1730 pressure transducer and Campbell Scientific (CS) CR1000 data logger. Stage is given as DN. To derive discharge (Q), a stage-discharge rating curve was developed using 18 dilution experiments of 10% fluorescein and a Turner Designs Cyclops7 fluorometer linked to a CS CR10X datalogger. Rating curve observations covered the lowermost 50% of stage values recorded, and uncertainty in Q is estimated at 10-15%. The non-linear exponential stage-discharge relationship was given as: Q = 0.2839.e^(5.55397.S). Discharge is in m^3/s. Data extends from 14th May (DOY134) to 13th November (DOY317), and time is given as decimal-day format (DOY135.5 = 12:00 midday on DOY135).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_883419
institution PANGAEA
language en
publishDate 2017
publisher PANGAEA
record_format pangaea
spellingShingle Meltwater stage and discharge from outlet stream from Khumbu Glacier, Everest region, Nepal, between 14th May and 13th November 2014
Irvine-Fynn, Tristram D L
Porter, P R
Rowan, Ann V
Quincey, Duncan J
Gibson, Morgan J
Bridge, J W
Watson, C Scott
Hubbard, Alun L
Glasser, Neil F
DATE/TIME; Day of the year; KhumbuGlacier_outflow; Nepal; RGS; River discharge; River gauging station; Sensor reading
A hydrological monitoring station for Khumbu Glacier, Nepal, was established in a stable reach of the sole outflow channel at 4930 m a.s.l.. at approximately 27°56'02"N 86°48'44"E where meltwater breaches the lateral/terminal moraine ridge. Average water stage (S) was recorded at 30 min intervals using a Druck PDCR1730 pressure transducer and Campbell Scientific (CS) CR1000 data logger. Stage is given as DN. To derive discharge (Q), a stage-discharge rating curve was developed using 18 dilution experiments of 10% fluorescein and a Turner Designs Cyclops7 fluorometer linked to a CS CR10X datalogger. Rating curve observations covered the lowermost 50% of stage values recorded, and uncertainty in Q is estimated at 10-15%. The non-linear exponential stage-discharge relationship was given as: Q = 0.2839.e^(5.55397.S). Discharge is in m^3/s. Data extends from 14th May (DOY134) to 13th November (DOY317), and time is given as decimal-day format (DOY135.5 = 12:00 midday on DOY135).
title Meltwater stage and discharge from outlet stream from Khumbu Glacier, Everest region, Nepal, between 14th May and 13th November 2014
topic DATE/TIME; Day of the year; KhumbuGlacier_outflow; Nepal; RGS; River discharge; River gauging station; Sensor reading
url https://doi.org/10.1594/PANGAEA.883419