AbstractDiurnal variations in water vapour in the Baltic Sea region are examined using BaltAn65+ and NCEP-CFSR reanalyses of summer (JJA) data for the period 1979–2005. A systematic difference between precipitable water (PW) diurnal variability above the land and the water is revealed. Above the land, PW diurnal variability has minimal values at 00 and 06 UTC, as in previous studies, whereas above the water, the minima are at 12 and 18 UTC. Diurnal variability in the vertical humidity profile is controlled by turbulent mixing and the diurnal behaviour of sea breezes. The impacts and proportions of diurnal variability of humidity are evaluated at different vertical levels
Water vapour is the most important greenhouse gas, contributing to about 60% of the natural greenhou...
Marine meteorological conditions and air-sea exchange processes over the northern Baltic Sea were st...
Sea Surface Temperature (SST) maps derived from NOAA weathersatellites for the period 1990-2004 were...
Diurnal variations in water vapour in the Baltic Sea region are examined using BaltAn65+ and NCEP-CF...
Diurnal variations in water vapour in the Baltic Sea region are examined using BaltAn65+ and NCEP-CF...
AbstractDiurnal variations in water vapour in the Baltic Sea region are examined using BaltAn65+ and...
Diurnal variations in the Integrated Precipitable Water Vapour (IPWV) are studied from GPS observati...
The present study examines the seasonal and decadal changes of the variance of the synoptic (periods...
International audienceCoastal seas and estuarine systems are highly variable in both time and space ...
Satellite measurements provide synoptic view of sea surface temperature (SST) and can be used to tra...
SummarySatellite measurements provide synoptic view of sea surface temperature (SST) and can be used...
In coastal and semi-enclosed seas, the mean local sea level can significantly influence the magnitud...
Coastal sea-level trends in the Baltic Sea display decadal-scale variations around a long-term cente...
The Baltic and North Seas Climatology (BNSC) presented here is a new climatology calculated solely f...
In order to investigate the energy and water balance of the Baltic Sea and its catchment area, the c...
Water vapour is the most important greenhouse gas, contributing to about 60% of the natural greenhou...
Marine meteorological conditions and air-sea exchange processes over the northern Baltic Sea were st...
Sea Surface Temperature (SST) maps derived from NOAA weathersatellites for the period 1990-2004 were...
Diurnal variations in water vapour in the Baltic Sea region are examined using BaltAn65+ and NCEP-CF...
Diurnal variations in water vapour in the Baltic Sea region are examined using BaltAn65+ and NCEP-CF...
AbstractDiurnal variations in water vapour in the Baltic Sea region are examined using BaltAn65+ and...
Diurnal variations in the Integrated Precipitable Water Vapour (IPWV) are studied from GPS observati...
The present study examines the seasonal and decadal changes of the variance of the synoptic (periods...
International audienceCoastal seas and estuarine systems are highly variable in both time and space ...
Satellite measurements provide synoptic view of sea surface temperature (SST) and can be used to tra...
SummarySatellite measurements provide synoptic view of sea surface temperature (SST) and can be used...
In coastal and semi-enclosed seas, the mean local sea level can significantly influence the magnitud...
Coastal sea-level trends in the Baltic Sea display decadal-scale variations around a long-term cente...
The Baltic and North Seas Climatology (BNSC) presented here is a new climatology calculated solely f...
In order to investigate the energy and water balance of the Baltic Sea and its catchment area, the c...
Water vapour is the most important greenhouse gas, contributing to about 60% of the natural greenhou...
Marine meteorological conditions and air-sea exchange processes over the northern Baltic Sea were st...
Sea Surface Temperature (SST) maps derived from NOAA weathersatellites for the period 1990-2004 were...