The secular record of annual mean temperatures of Bremen shows that inhomogeneities - especially caused by station transfers - lead to serious problems concerning the interpretation of climatic trends or fluctuations. Especially two transfers of the meteorological observing station in Bremen within our century - 1935/36 and 1978 - caused significant inhomogeneities, well documented by parallel measurements for several years. Obviously the stagnation of the temperature level of the original data set is a result of these transfers. The homogenized record version reveals a significant warming trend of about 1 Kelvin within the last century
Germany's national meteorological service (Deutscher Wetterdienst) is responsible for monitoring cli...
Climate changes and the urban climate of the 'green city' Hamburg and its metropolitan region are an...
In reference to the publication Long-term meteorological measurements at Zagreb: 1862 – 1990 (Penzar...
Over several decades the physician and astronomer Wilhelm Olbers (1758--1840) has consistently made ...
Air temperatures increase systematically since the middle of the 19th century and this increase beco...
Long-term climate registrations are of great importance for climate modelling and prediction. The ti...
Uninterrupted series of annual mean temperatures from 72 European observatories have been processed....
Day-to-day temperature variability is investigated in eight European series of daily mean temperatur...
This paper deals with the analysis of long-term temperature changes in Europe in the period 1957-200...
We took daily near-surface air temperature data from across Europe to calculate a series of 12 biol...
We analysed long-term temperature trends based on 12 homogenised series of monthly temperature data ...
Long-term changes in the persistence of atmospheric circulation (measured by the mean residence time...
In the University campus Klementinum in Prague air temperatures have been recorded every day since 1...
Provides a method which allows the detection of an abrupt climatic change and which localizes approx...
In Part 1, we review the uncertainties associated with combining land and marine instrumental record...
Germany's national meteorological service (Deutscher Wetterdienst) is responsible for monitoring cli...
Climate changes and the urban climate of the 'green city' Hamburg and its metropolitan region are an...
In reference to the publication Long-term meteorological measurements at Zagreb: 1862 – 1990 (Penzar...
Over several decades the physician and astronomer Wilhelm Olbers (1758--1840) has consistently made ...
Air temperatures increase systematically since the middle of the 19th century and this increase beco...
Long-term climate registrations are of great importance for climate modelling and prediction. The ti...
Uninterrupted series of annual mean temperatures from 72 European observatories have been processed....
Day-to-day temperature variability is investigated in eight European series of daily mean temperatur...
This paper deals with the analysis of long-term temperature changes in Europe in the period 1957-200...
We took daily near-surface air temperature data from across Europe to calculate a series of 12 biol...
We analysed long-term temperature trends based on 12 homogenised series of monthly temperature data ...
Long-term changes in the persistence of atmospheric circulation (measured by the mean residence time...
In the University campus Klementinum in Prague air temperatures have been recorded every day since 1...
Provides a method which allows the detection of an abrupt climatic change and which localizes approx...
In Part 1, we review the uncertainties associated with combining land and marine instrumental record...
Germany's national meteorological service (Deutscher Wetterdienst) is responsible for monitoring cli...
Climate changes and the urban climate of the 'green city' Hamburg and its metropolitan region are an...
In reference to the publication Long-term meteorological measurements at Zagreb: 1862 – 1990 (Penzar...