Linking North Atlantic ocean-atmosphere teleconnection patterns and hydrogeological responses in temperate groundwater systems

Holman, I.P.; Rivas-Casado, M.; Howden, N.J.K.; Bloomfield, J.P. ORCID: https://orcid.org/0000-0002-5730-1723; Williams, A.T.. 2009 Linking North Atlantic ocean-atmosphere teleconnection patterns and hydrogeological responses in temperate groundwater systems. Hydrological Processes, 23. 3123-3126. 10.1002/hyp.7466

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Abstract/Summary

Climate signals exhibit periodicity over a range of frequencies (e.g. diurnal, seasonal, annual and longer term climate phenomena) that are modified as they propagate through the terrestrial water cycle. Much of both our present understanding and modelling of temperate hydrological and hydrogeological systems relies on the preservation of high-frequency signals (e.g. diurnal and seasonal cycles: Holman et al., 2009; Alley et al., 2002). However, there is evidence to suggest that low-frequency oscillations in rainfall, temperature and evapotranspiration are linked to the El Ni ˜no Southern Oscillation (Jones and Banner, 2003), Pacific Decadal Oscillation (Gurdak et al., 2007), North Atlantic Oscillation (NAO) (Schroder and Rosbjerg, 2004; Qian and Saunders, 2003) and other ocean–climate cycles.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1002/hyp.7466
Programmes:	BGS Programmes 2009 > Groundwater science
ISSN:	0885-6087
Additional Keywords:	GroundwaterBGS, Groundwater, Climate change, Environmental change
NORA Subject Terms:	Hydrology
Related URLs:	http://www.bgs.ac.uk/research/groundwate...
Date made live:	08 Oct 2009 12:28 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/8247

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