✦ LIBER ✦

Relationship of extreme dry spells in Eastern Mediterranean with large-scale circulation

✍ Scribed by C. Oikonomou; H. A. Flocas; M. Hatzaki; A. Nisantzi; D. N. Asimakopoulos

Publisher: Springer
Year: 2009
Tongue: English
Weight: 794 KB
Volume: 100
Category: Article
ISSN: 1434-4483
DOI: 10.1007/s00704-009-0171-4

No coin nor oath required. For personal study only.

📜 SIMILAR VOLUMES

Variability of extreme temperature event

Variability of extreme temperature events in south–central Europe during the 20th century and its relationship with large-scale circulation

✍ Peter Domonkos; Jan Kyselý; Katarzyna Piotrowicz; Predrag Petrovic; Tanja Likso 📂 Article 📅 2003 🏛 John Wiley and Sons 🌐 English ⚖ 378 KB

## Abstract The variability of winter extreme low‐temperature events and summer extreme high‐temperature events was investigated using daily temperature series (1901–98) from 11 sites in central and southern Europe. An extreme temperature event (EXTE) is defined by various threshold values of daily

Local Circulation Diurnal Patterns and T

Local Circulation Diurnal Patterns and Their Relationship with Large-Scale Flows in a Coastal Area of the Tyrrhenian Sea

✍ Igor Petenko; Giangiuseppe Mastrantonio; Angelo Viola; Stefania Argentini; Lucia 📂 Article 📅 2011 🏛 Springer 🌐 English ⚖ 797 KB

Climatic changes in Estonia during the s

Climatic changes in Estonia during the second half of the 20th century in relationship with changes in large-scale atmospheric circulation

✍ J. Jaagus 📂 Article 📅 2005 🏛 Springer 🌐 English ⚖ 294 KB

An analysis of mid-summer rainfall occur

An analysis of mid-summer rainfall occurrence in eastern China and its relationship with large-scale warming using generalized linear models

✍ Yi Wang; Zhongwei Yan; Richard E. Chandler 📂 Article 📅 2009 🏛 John Wiley and Sons 🌐 English ⚖ 342 KB

## Abstract Daily rainfall occurrence in mid‐summer (July and August) in eastern China was analyzed using binomial generalized linear models based on observations at 303 stations during 1961–2007. The models include an intraseasonal variation, previous days' rainfall to represent the Markov chain s