Decadal climate variability and the spatial organization of deep hydrological drought

Empirical Orthogonal Function (EOF), wavelet, and wavelet coherence analysis of baseflow time-series from 126 streamgauges (record-length > 50 years; small and mid-size watersheds) in the US South Atlantic (USSA) region reveal three principal modes of space-time variability: (1) a region-wide dom...

Full description

Bibliographic Details
Main Authors: Ana P Barros, Jared L Hodes, Malarvizhi Arulraj
Format: Article
Language:English
Published: IOP Publishing 2017-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/aa81de
_version_ 1797748244586954752
author Ana P Barros
Jared L Hodes
Malarvizhi Arulraj
author_facet Ana P Barros
Jared L Hodes
Malarvizhi Arulraj
author_sort Ana P Barros
collection DOAJ
description Empirical Orthogonal Function (EOF), wavelet, and wavelet coherence analysis of baseflow time-series from 126 streamgauges (record-length > 50 years; small and mid-size watersheds) in the US South Atlantic (USSA) region reveal three principal modes of space-time variability: (1) a region-wide dominant mode tied to annual precipitation that exhibits non-stationary decadal variability after the mid 1990s concurrent with the warming of the AMO (Atlantic Multidecadal Oscillation); (2) two spatial modes, east and west of the Blue Ridge, exhibiting nonstationary seasonal to sub-decadal variability before and after 1990 attributed to complex nonlinear interactions between ENSO and AMO impacting precipitation and recharge; and (3) deep (decadal) and shallow (< 6 years) space-time modes of groundwater variability separating basins with high and low annual mean baseflow fraction (MBF) by physiographic region. The results explain the propagation of multiscale climate variability into the regional groundwater system through recharge modulated by topography, geomorphology, and geology to determine the spatial organization of baseflow variability at decadal (and longer) time-scales, that is, deep hydrologic drought. Further, these findings suggest potential for long-range predictability of hydrological drought in small and mid-size watersheds, where baseflow is a robust indicator of nonstationary yield capacity of the underlying groundwater basins. Predictive associations between climate mode indices and deep baseflow (e.g. persistent decreases of the decadal-scale components of baseflow during the cold phase of the AMO in the USSA) can be instrumental toward improving forecast lead-times and long-range mitigation of severe drought.
first_indexed 2024-03-12T16:02:08Z
format Article
id doaj.art-f00e6cd8812d4445a2ad2ae9fd34b0ff
institution Directory Open Access Journal
issn 1748-9326
language English
last_indexed 2024-03-12T16:02:08Z
publishDate 2017-01-01
publisher IOP Publishing
record_format Article
series Environmental Research Letters
spelling doaj.art-f00e6cd8812d4445a2ad2ae9fd34b0ff2023-08-09T14:36:12ZengIOP PublishingEnvironmental Research Letters1748-93262017-01-01121010400510.1088/1748-9326/aa81deDecadal climate variability and the spatial organization of deep hydrological droughtAna P Barros0Jared L Hodes1Malarvizhi Arulraj2Duke University , 2453 CIEMAS, Box 90287, Durham, NC 27708, United States of America; Author to whom any correspondence should be addressed.Duke University , 2453 CIEMAS, Box 90287, Durham, NC 27708, United States of AmericaDuke University , 2453 CIEMAS, Box 90287, Durham, NC 27708, United States of AmericaEmpirical Orthogonal Function (EOF), wavelet, and wavelet coherence analysis of baseflow time-series from 126 streamgauges (record-length > 50 years; small and mid-size watersheds) in the US South Atlantic (USSA) region reveal three principal modes of space-time variability: (1) a region-wide dominant mode tied to annual precipitation that exhibits non-stationary decadal variability after the mid 1990s concurrent with the warming of the AMO (Atlantic Multidecadal Oscillation); (2) two spatial modes, east and west of the Blue Ridge, exhibiting nonstationary seasonal to sub-decadal variability before and after 1990 attributed to complex nonlinear interactions between ENSO and AMO impacting precipitation and recharge; and (3) deep (decadal) and shallow (< 6 years) space-time modes of groundwater variability separating basins with high and low annual mean baseflow fraction (MBF) by physiographic region. The results explain the propagation of multiscale climate variability into the regional groundwater system through recharge modulated by topography, geomorphology, and geology to determine the spatial organization of baseflow variability at decadal (and longer) time-scales, that is, deep hydrologic drought. Further, these findings suggest potential for long-range predictability of hydrological drought in small and mid-size watersheds, where baseflow is a robust indicator of nonstationary yield capacity of the underlying groundwater basins. Predictive associations between climate mode indices and deep baseflow (e.g. persistent decreases of the decadal-scale components of baseflow during the cold phase of the AMO in the USSA) can be instrumental toward improving forecast lead-times and long-range mitigation of severe drought.https://doi.org/10.1088/1748-9326/aa81delarge-scale groundwaterbaseflow and recession analysisclimate and precipitation variability
spellingShingle Ana P Barros
Jared L Hodes
Malarvizhi Arulraj
Decadal climate variability and the spatial organization of deep hydrological drought
Environmental Research Letters
large-scale groundwater
baseflow and recession analysis
climate and precipitation variability
title Decadal climate variability and the spatial organization of deep hydrological drought
title_full Decadal climate variability and the spatial organization of deep hydrological drought
title_fullStr Decadal climate variability and the spatial organization of deep hydrological drought
title_full_unstemmed Decadal climate variability and the spatial organization of deep hydrological drought
title_short Decadal climate variability and the spatial organization of deep hydrological drought
title_sort decadal climate variability and the spatial organization of deep hydrological drought
topic large-scale groundwater
baseflow and recession analysis
climate and precipitation variability
url https://doi.org/10.1088/1748-9326/aa81de
work_keys_str_mv AT anapbarros decadalclimatevariabilityandthespatialorganizationofdeephydrologicaldrought
AT jaredlhodes decadalclimatevariabilityandthespatialorganizationofdeephydrologicaldrought
AT malarvizhiarulraj decadalclimatevariabilityandthespatialorganizationofdeephydrologicaldrought