1981
DOI: 10.1016/0022-1694(81)90211-0
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Delimitation of New Zealand hydrologic regions

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Cited by 136 publications
(78 citation statements)
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“…The (broadly speaking) statistical distribution of hydrologic states and fluxes over a larger time-and space scale has been referred to as a system's regime (Pickup and Warner, 1976;Mosley, 1981;Magilligan and Nislow, 2005). This structure has been investigated through the prism of signatures including the flood frequency curve (e.g., Robinson and Sivapalan, 1997), water balance partitioning Harman et al, 2011;Sivapalan et al, 2011a), flow duration curve Yaeger et al, 2012;Ye et al, 2012), recession curve (e.g., Wittenberg, 2003), preferred states in the soil moisture distribution (e.g., Western and Grayson, 2001), and seasonal variations in the fluxes measured at an eddy-flux tower .…”
Section: Variation Across Time: Regimes and Filteringmentioning
confidence: 99%
“…The (broadly speaking) statistical distribution of hydrologic states and fluxes over a larger time-and space scale has been referred to as a system's regime (Pickup and Warner, 1976;Mosley, 1981;Magilligan and Nislow, 2005). This structure has been investigated through the prism of signatures including the flood frequency curve (e.g., Robinson and Sivapalan, 1997), water balance partitioning Harman et al, 2011;Sivapalan et al, 2011a), flow duration curve Yaeger et al, 2012;Ye et al, 2012), recession curve (e.g., Wittenberg, 2003), preferred states in the soil moisture distribution (e.g., Western and Grayson, 2001), and seasonal variations in the fluxes measured at an eddy-flux tower .…”
Section: Variation Across Time: Regimes and Filteringmentioning
confidence: 99%
“…For consistency throughout our paper, we use the former meaning of the term. Mosley (1981) derived hydrologic regionalizations via cluster analyses of hydrologic data. Others (Singh 1971, Cunnane 1988 have predicted flow for regions with reasonably homogeneous flow characteristics by applying regionally representative flows to all catchments in those regions.…”
Section: Predicting Hydrologic Reference Conditionsmentioning
confidence: 99%
“…The location and scale of individual flood series can be described by two standardized statistics: the specific mean annual flood, QSP, and the coefficient of variation, CV (Mosley, 1981). QSP has an attractive intuitive meaning and can be described as the spatial intensity of the mean annual maximum flood.…”
Section: Derivation Of Basin Clustersmentioning
confidence: 99%