Title
Summertime precipitation deficits in the southern Peruvian highlands since 1964
Date Issued
01 September 2019
Access level
open access
Resource Type
journal article
Author(s)
Imfeld N.
Christian Barreto Schuler
Jacques-Coper M.
Sedlmeier K.
Gubler S.
Brönnimann S.
Publisher(s)
John Wiley and Sons Ltd
Abstract
Precipitation deficits remain a concern to the rural population in the southern Peruvian highlands and knowledge about their occurrence is lacking because of scarce data availability. For mountainous regions with sparse station networks, reanalyses can provide valuable information; however, known limitations in reproducing precipitation are aggravated due to unresolved topographical effects. In this study, we assess in a first step the representation of precipitation during the rainy season (January–February–March) in seven reanalysis data sets in comparison to a newly generated gridded precipitation data set for Peru. In a second step, we assess summer precipitation deficits in Peru during the second half of the 20th century. In the reanalyses data sets, we find biases strongly influenced by the topography of the models and low correlations for the rainy season. Thus, reanalyses do not solve the problem of data scarcity for this region either. Furthermore, we confirm that El Niño is not a sufficient stratification criterion for precipitation deficits during the rainy season (JFM) in the southern Peruvian highlands. Based on observational records and reanalyses, a considerable fraction of inter-annual variability of precipitation can be explained through upper-tropospheric zonal wind anomalies. Westerly wind anomalies, often related to the warming of the troposphere during an El Niño event, lead to dry conditions, but not all El Niño events produce these westerly wind anomalies. Atmospheric simulations indicate differences between precipitation deficits in central Pacific and eastern Pacific El Niño flavours, which cannot be addressed in observations due to reduced record length: Droughts in the southern Peruvian Andes during eastern Pacific El Niño events seem to be related to a stronger warming in the troposphere above the central Pacific ocean, whereas this is not the case for droughts during central Pacific El Niño events. These results, however, need to be further corroborated by model studies and palaeoclimatological research.
Start page
4497
End page
4513
Volume
39
Issue
11
Language
English
OCDE Knowledge area
Meteorología y ciencias atmosféricas
Investigación climática
Subjects
DOI
Scopus EID
2-s2.0-85065213748
Source
International Journal of Climatology
ISSN of the container
08998418
Sponsor(s)
This work was funded by the SDC under project CLIMANDES-2. We acknowledge the support of the World Meteorological Organization (WMO) through the project “Servicios CLIMáticos con énfasis en los ANdes en apoyo a las DEcisioneS” (CLIMANDES), Project No. 7F-08453.02 between the Swiss Agency for Development and Cooperation (SDC) and the WMO. S.B. acknowledges funding from the SDC/SNF project DECADE and EU-FP7 project ERA-CLIM2. M.J.C. acknowledges CONICYT-Chile through grants PAI79160105 and FONDAP15110009.
Sources of information:
Directorio de Producción Científica
Scopus
Servicio Nacional de Meteorología e Hidrología del Perú