## Abstract The Iberian Peninsula precipitation and river flow regimes are characterized by large values of inter‐annual variability, with large disparities between wet and dry years, especially in southern Iberia. This situation is a major problem for water resources management in general, and for
Trends of precipitation over the Iberian Peninsula and the North Atlantic Oscillation under climate change conditions
✍ Scribed by Concepción Rodríguez-Puebla; Susana Nieto
- Publisher
- John Wiley and Sons
- Year
- 2009
- Tongue
- English
- Weight
- 621 KB
- Volume
- 30
- Category
- Article
- ISSN
- 0899-8418
- DOI
- 10.1002/joc.2035
No coin nor oath required. For personal study only.
✦ Synopsis
Abstract
The trends of precipitation over the Iberian Peninsula (IP) and the North Atlantic Oscillation (NAO) index from December to March are compared using observations and model simulations from the Coupled Model Intercomparison Project phase 3 (CMIP3). The evaluation is performed in two multi‐models as derived by averaging simulations corresponding to two experiments: one represents climate in the 20th century (20C3M) and the other the scenario with medium forcing IPCC SRES A1B in the 21st century. The NAO index shows a trend to more positive phases and precipitation tends to decrease in the case of observations, with greater significance in the NAO than in precipitation. The simulations in the 20th century underestimate the trend both in the NAO and in precipitation compared to observations. The multi‐model in the 21st century indicates a change in the NAO regimes to being more positive; this leads to a reduction of precipitation over the IP. To explain the precipitation trend changes we consider the response of precipitation to the NAO, the regression between sea level pressure (SLP) over the Euro‐Atlantic area onto precipitation averaged over the IP and the composite of precipitation for years with greater and lower NAO. Copyright © 2009 Royal Meteorological Society
📜 SIMILAR VOLUMES
## Abstract Variations in precipitation in Yorkshire, UK, are linked to large‐scale atmospheric circulation using the North Atlantic Oscillation (NAO) index, objective Lamb weather types, and long‐term seasonal and annual precipitation indices at seven sites. Since the 1960s, a significant decrease
## Abstract The variability of Seine River flow (France) was investigated using daily time series over the period of 1950–2008. The study aimed at characterizing the dominant modes explaining the variability of flow and at investigating their possible link with the North Atlantic Oscillation (NAO)