In this study, we consider the historical climatological time series available in the meteorological yearbooks of the Royal Hungarian Central Institute of Meteorology and Earth Magnetism, first published in 1871. Data quality improvement of historical data includes the homogenization process with outlier checks and data gap filling by applying the MASH software. We investigated 13 stations from the Carpathian Region having the most complete monthly temperature and precipitation time series for the period of 1871–1918 and 8 stations with fog observations (1886–1916). First, statistical tests were conducted to compare the main statistics of the historical datasets (1871–1918) with current data (1971–2020). The sources of the current data are ...
In this article we analyse the evolution in time of extreme temperatures significant for Romania wit...
The aim of our study is to analyse the spatial patterns and temporal trends of average and extreme p...
Dates of mean daily temperature transitions of 0°C, 5°C, 10°C and respective season lengths are amon...
The Carpathians are the largest mountain range in Europe and they represent a geographic barrier bet...
To investigate the climate of the Carpathian Region (17°-27°E; 44°-50°N), the European Commission la...
The variability of winter mean precipitation as observed at 14 Romanian rain gauge stations from 190...
The aim of this paper is to investigate the statistical aspects of multiannual variability of precip...
The variability of winter mean precipitation as observed at 14 Romanian rain gauge stations From 190...
Covering a period of 23 years, the Timişoara (in historical Banat region; today SW-Romania) series i...
The spatial and temporal variability of winter precipitation and its links to the large-scale atmosp...
The Romanian Carpathians are located at the confluence of three major atmospheric pressure fields: t...
<p class="xl27">Changes in daily extreme precipitations have been identified in many studies conduct...
Many studies link the observed changes in local climate to the variations in the atmospheric circula...
Precipitation is the major atmospheric source of surface water, thus, in order to build appropriate ...
Daily records of nine meteorological variables covering the interval 1961-2013 were used in order to...
In this article we analyse the evolution in time of extreme temperatures significant for Romania wit...
The aim of our study is to analyse the spatial patterns and temporal trends of average and extreme p...
Dates of mean daily temperature transitions of 0°C, 5°C, 10°C and respective season lengths are amon...
The Carpathians are the largest mountain range in Europe and they represent a geographic barrier bet...
To investigate the climate of the Carpathian Region (17°-27°E; 44°-50°N), the European Commission la...
The variability of winter mean precipitation as observed at 14 Romanian rain gauge stations from 190...
The aim of this paper is to investigate the statistical aspects of multiannual variability of precip...
The variability of winter mean precipitation as observed at 14 Romanian rain gauge stations From 190...
Covering a period of 23 years, the Timişoara (in historical Banat region; today SW-Romania) series i...
The spatial and temporal variability of winter precipitation and its links to the large-scale atmosp...
The Romanian Carpathians are located at the confluence of three major atmospheric pressure fields: t...
<p class="xl27">Changes in daily extreme precipitations have been identified in many studies conduct...
Many studies link the observed changes in local climate to the variations in the atmospheric circula...
Precipitation is the major atmospheric source of surface water, thus, in order to build appropriate ...
Daily records of nine meteorological variables covering the interval 1961-2013 were used in order to...
In this article we analyse the evolution in time of extreme temperatures significant for Romania wit...
The aim of our study is to analyse the spatial patterns and temporal trends of average and extreme p...
Dates of mean daily temperature transitions of 0°C, 5°C, 10°C and respective season lengths are amon...