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Spatial patterns and regimes of daily precipitation in Iran in relation to large‐scale atmospheric circulation
Author(s) -
Raziei Tayeb,
Mofidi Abbas,
Santos João A.,
Bordi Isabella
Publication year - 2011
Publication title -
international journal of climatology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.58
H-Index - 166
eISSN - 1097-0088
pISSN - 0899-8418
DOI - 10.1002/joc.2347
Subject(s) - climatology , anticyclone , precipitation , environmental science , atmospheric circulation , trough (economics) , troposphere , spatial ecology , spatial distribution , varimax rotation , common spatial pattern , synoptic scale meteorology , atmospheric sciences , geology , geography , meteorology , ecology , statistics , remote sensing , mathematics , cronbach's alpha , descriptive statistics , biology , economics , macroeconomics
The relationships between large‐scale atmospheric circulation types and seasonal regimes of daily precipitation over Iran are assessed using daily precipitation from a high‐resolution gridded dataset provided by the Asian Precipitation‐Highly Resolved Observational Data Integration Towards the Evaluation of Water Resources (APHRODITE) Project. Regional spatial modes of daily precipitation variability were identified by S‐mode Principal Component Analysis (PCA) with Varimax rotation, applied to the subset of days when at least 10% of all grid‐points over Iran received precipitation ≥ 5 mm. The study refers to the period 1961–2004 and is carried out for each season (excluding summer) separately. To characterize the dynamical features associated with each regional precipitation regime (PR), composites of daily atmospheric fields are computed by only averaging days with rotated PCA scores ≥ 1.5 (strong positive phase). In autumn and winter, Iran is divided into five PRs, while four PRs are identified in spring. Results suggest that the spatial distribution of precipitation over Iran is largely governed by the geographical position of both the mid‐tropospheric trough over the Middle East and the Arabian anticyclone. In fact, in almost all PRs, the trough, as a pre‐conditioning factor, leads to regional‐scale ascending motions, whereas the Arabian anticyclone induces low‐tropospheric moisture transports from southern water bodies into the cyclonic systems near Iran, triggering rain‐generating conditions. Copyright © 2011 Royal Meteorological Society