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Monthly mean pressure reconstruction for the Late Maunder Minimum Period (AD 1675–1715)

✍ Scribed by J. Luterbacher; R. Rickli; C. Tinguely; E. Xoplaki; E. Schüpbach; D. Dietrich; J. Hüsler; M. Ambühl; C. Pfister; P. Beeli; U. Dietrich; A. Dannecker; T.D. Davies; P.D. Jones; V. Slonosky; A.E.J. Ogilvie; P. Maheras; F. Kolyva-Machera; J. Martin-Vide; M. Barriendos; M.J. Alcoforado; M.F. Nunes; T. Jónsson; R. Glaser; J. Jacobeit; C. Beck; A. Philipp; U. Beyer; E. Kaas; T. Schmith; L. Bärring; P. Jönsson; L. Rácz; H. Wanner

Book ID: 101323455
Publisher: John Wiley and Sons
Year: 2000
Tongue: English
Weight: 254 KB
Volume: 20
Category: Article
ISSN: 0899-8418
DOI: 10.1002/1097-0088(200008)20:10<1049::aid-joc521>3.0.co;2-6

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The Late Maunder Minimum (1675–1715) – A

The Late Maunder Minimum (1675–1715) – A Key Period forStudying Decadal Scale Climatic Change in Europe

✍ J. Luterbacher; R. Rickli; E. Xoplaki; C. Tinguely; C. Beck; C. Pfister; H. Wann 📂 Article 📅 2001 🏛 Springer 🌐 English ⚖ 292 KB

Monthly mean pressure reconstructions fo

Monthly mean pressure reconstructions for Europe for the 1780–1995 period

✍ Jones, P.D.; Davies, T.D.; Lister, D.H.; Slonosky, V.; Jónsson, T.; Bärring, L.; 📂 Article 📅 1999 🏛 John Wiley and Sons 🌐 English ⚖ 413 KB

Monthly grid-point pressure data are reconstructed from station records of pressure for Europe since 1780. The region encompasses 35-70 o N to 30 o W-40 o E. The reconstructions are based on a principal components regression technique, which relates surface pressure patterns to those of the station