The influences of the Southern and North Atlantic Oscillations on climatic surface variables in Turkey

Karabork M., KAHYA E., Karaca M.

HYDROLOGICAL PROCESSES, vol.19, no.6, pp.1185-1211, 2005 (SCI-Expanded) identifier identifier

  • Publication Type: Article / Article
  • Volume: 19 Issue: 6
  • Publication Date: 2005
  • Doi Number: 10.1002/hyp.5560
  • Journal Indexes: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Page Numbers: pp.1185-1211
  • Istanbul Technical University Affiliated: No


In this study, Turkish climatic variables (precipitation, stream flow and maximum and minimum temperatures) were first analysed in association with both the Southern Oscillation (SO) and the North Atlantic Oscillation (NAO). The relationships between Turkish maximum and minimum monthly temperatures and the extreme phases of the SO (El Ni (n) over tildeo and La Ni (n) over tildea events) were examined. The results of this analysis showed that relationships between Turkish monthly maximum temperatures and El Ni (n) over tildeo and La Ni (n) over tildea contain some complexity still to be identified, because both events produce a signal indicating a correspondence with cold anomalies in the aggregate composites. A relationship between turkish minimum temperatures and El Ni (n) over tildeo was detected in western Anatolia, whereas there was no significant and consistent signal associated with La Ni (n) over tildea. Moreover a series of cross-correlation analyses was carried out to demonstrate the teleconnections between the climatic variables and both the NAO and SO. The NAO during winter was found to influence precipitation and stream-flow patterns. In contrast temperature patterns appeared to be less sensitive to the NAO. Furthermore, lag-correlation results indicated a prediction potential for both precipitation and stream-flow variables in connection with the NAO. Simultaneous and time-lag correlations between the climatic variables and the SO index, in general, indicated weaker relationships in comparison with those for the NAO. These analyses also showed that the influences of the SO on Turkish temperature data are negligible. The outcomes were presented in conjunction with an explanation regarding physical mechanisms behind the implied teleconnections. Copyright (c) 2004 John Wiley & Sons, Ltd.