Monthly grid-point pressure data are reconstructed from station records of pressure for Europe since 1780. The region encompasses 35-70°N to 30°W-40°E. The reconstructions are based on a principal components regression technique, which relates surface pressure patterns to those of the station pressure data. The relationships are derived over a calibration period (1936-1995) and the results tested with independent data (the verification period, 1881-1935). The reconstructions are of excellent quality, although this is slightly lower for regions with poor station coverage in the early years, particularly during the summer months. The reconstructions are compared with other monthly mean pressure maps produced by Lamb and Johnson (1966) for the...
We present seasonal precipitation reconstructions for European land areas (30°W to 40°E/30–71°N; giv...
It has been known for some time that the potential exists to construct a long daily series of surfac...
Local to regional climate anomalies are to a large extent determined by the state of the atmospheric...
The Late Maunder Minimum (LMM; 1675–1715) delineates a period with marked climate variability within...
The Late Maunder Minimum (LMM; 1675-1715) delineates a period with marked climate variability within...
The development of a daily historical European-North Atlantic mean sea level pressure dataset (EMSLP...
Measurements of wind strength and direction abstracted from European ships' logbooks during the rece...
The development of a daily historical European–North Atlantic mean sea level pressure dataset (EMSLP...
International audienceMeasurements of wind strength and direction abstracted from European ships' lo...
© 2019 by the authors. Licensee MDPI, Basel, Switzerland. The relationship between Southern Hemisphe...
Monthly temperature series for Central Europe back to AD 1500 are developed from documentary index s...
Seasonal climate reconstructions of sea level pressure and temperature for the North Atlantic region...
In a regional analysis the removal of the globally present semi-diurnal pressure signal could be nec...
This paper presents a comparison of principal component (PC) regression and regularized expectation ...
Long series of monthly surface pressure observations are analysed from the 1770s to 1995, using empi...
We present seasonal precipitation reconstructions for European land areas (30°W to 40°E/30–71°N; giv...
It has been known for some time that the potential exists to construct a long daily series of surfac...
Local to regional climate anomalies are to a large extent determined by the state of the atmospheric...
The Late Maunder Minimum (LMM; 1675–1715) delineates a period with marked climate variability within...
The Late Maunder Minimum (LMM; 1675-1715) delineates a period with marked climate variability within...
The development of a daily historical European-North Atlantic mean sea level pressure dataset (EMSLP...
Measurements of wind strength and direction abstracted from European ships' logbooks during the rece...
The development of a daily historical European–North Atlantic mean sea level pressure dataset (EMSLP...
International audienceMeasurements of wind strength and direction abstracted from European ships' lo...
© 2019 by the authors. Licensee MDPI, Basel, Switzerland. The relationship between Southern Hemisphe...
Monthly temperature series for Central Europe back to AD 1500 are developed from documentary index s...
Seasonal climate reconstructions of sea level pressure and temperature for the North Atlantic region...
In a regional analysis the removal of the globally present semi-diurnal pressure signal could be nec...
This paper presents a comparison of principal component (PC) regression and regularized expectation ...
Long series of monthly surface pressure observations are analysed from the 1770s to 1995, using empi...
We present seasonal precipitation reconstructions for European land areas (30°W to 40°E/30–71°N; giv...
It has been known for some time that the potential exists to construct a long daily series of surfac...
Local to regional climate anomalies are to a large extent determined by the state of the atmospheric...