A methodology for investigation of the seasonal evolution in proglacial hydrograph form
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A methodology for investigation of the seasonal evolution in proglacial hydrograph form. / Hannah, David M.; Gurnell, Angela M.; McGregor, Glenn R.
In: Hydrological Processes, Vol. 13, No. 16 SPEC. ISS., 01.11.1999, p. 2603-2621.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - A methodology for investigation of the seasonal evolution in proglacial hydrograph form
AU - Hannah, David M.
AU - Gurnell, Angela M.
AU - McGregor, Glenn R.
PY - 1999/11/1
Y1 - 1999/11/1
N2 - This paper advances an objective method of diurnal hydrograph classification as an aid to exploring changes in the hydrological functioning of glacierized catchments over the ablation season. The temporal sequencing of different hydrograph classes allows identification of seasonal evolution in hydrograph form and also assists delimitation of hydrologically-meaningful time periods of similar diurnal discharge response. The effectiveness of this approach is illustrated by applying it to two contrasting summer discharge records for a small cirque basin. By comparing the results with patterns of surface energy receipt and glacier ablation, the seasonally transient relative influences of: (i) surface meltwater production and (ii) meltwater routing and storage conditions within the intervening glacier drainage system in determining runoff are elucidated. The method successfully characterizes distinct seasonal-scale changes in the diurnal outflow hydrograph during the ablation-dominated 1995 melt season but is also able to reveal underlying trends and short-term fluctuations in the precipitation-dominated, poorly ablation-regulated 1996 melt season. The limitations and benefits of this hydrograph classification technique are evaluated.
AB - This paper advances an objective method of diurnal hydrograph classification as an aid to exploring changes in the hydrological functioning of glacierized catchments over the ablation season. The temporal sequencing of different hydrograph classes allows identification of seasonal evolution in hydrograph form and also assists delimitation of hydrologically-meaningful time periods of similar diurnal discharge response. The effectiveness of this approach is illustrated by applying it to two contrasting summer discharge records for a small cirque basin. By comparing the results with patterns of surface energy receipt and glacier ablation, the seasonally transient relative influences of: (i) surface meltwater production and (ii) meltwater routing and storage conditions within the intervening glacier drainage system in determining runoff are elucidated. The method successfully characterizes distinct seasonal-scale changes in the diurnal outflow hydrograph during the ablation-dominated 1995 melt season but is also able to reveal underlying trends and short-term fluctuations in the precipitation-dominated, poorly ablation-regulated 1996 melt season. The limitations and benefits of this hydrograph classification technique are evaluated.
KW - French pyrenees
KW - Hydro-climatological time series
KW - Hydrograph classification
KW - Meltwater runoff
KW - Snow and glacier hydrology
UR - http://www.scopus.com/inward/record.url?scp=0033374961&partnerID=8YFLogxK
U2 - 10.1002/(SICI)1099-1085(199911)13:16<2603::AID-HYP936>3.0.CO;2-5
DO - 10.1002/(SICI)1099-1085(199911)13:16<2603::AID-HYP936>3.0.CO;2-5
M3 - Article
AN - SCOPUS:0033374961
VL - 13
SP - 2603
EP - 2621
JO - Hydrological Processes
JF - Hydrological Processes
SN - 0885-6087
IS - 16 SPEC. ISS.
ER -