The daily and annual variation of temperature, humidity and wind velocity at same places in Sweden

ReportsMeteorologyClimate

Hourly observations from aerodroms have been used to calculate hourly means of the most important climatological variables. For those varibles showing a marked daily and annual variation isopleth diagrams have been analysed for air temperature, humidity and wind velocity. The results are given for …

 
Type: Report
Report Series: RMK 8
Author: Ericsson, B.
Published: Sep, 1978
Last updated:

Statistical forecasting of sea level changes in the Baltic.

ReportsMeteorologyClimate

By expanding sea level data from 6 Swedish observation stations inte empirical orthogonal functions a very simple picture of the response of the Baltic to atmospheric forcing is obtained. It is found that not less than 65.5 per cent of the total variance is due to a general rise or lowering of the …

 
Type: Report
Report Series: RMK 9
Author: Holmström, I., and Stokes, J.
Published: Sep, 1978
Last updated:

Some results from a joint Swedish-Finnish sea ice experiment, March, 1977.

ReportsMeteorologyClimate

A joint Swedish-Finnish sea-ice experiment was performed during March 1977. Measurements in the atmosphere, ice and sea were made during six days onboard the Finnish Research vessel Aranda stationed in the ice field in the Bay of Bothnia. During two days measurements were also carried out from the

 
Type: Report
Report Series: RMK 10
Author: Omstedt, A., and Sahlberg, J.
Published: Sep, 1978
Last updated:

Byggnadsindustrins väderberoende, seminarieuppsats i företagsekonomi, B-nivå.

ReportsMeteorology

 
Type: Report
Report Series: RMK 11
Author: Haag, T.
Published: 1978
Last updated:

A predictive numerical model of the Atmospheric Boundary Layer based on the Turbulent Energy Equation.

ReportsMeteorology

The interest in numerical modeling of the atmospheric boundary layer has grown considerably over the last decade. At SMHI and elsewhere boundary layer models find applicatoions in local forecasting, especially at airports, in air pollution diffusion and dispersion studies and in wind …

 
Type: Report
Report Series: RMK 13
Author: Bodin, S.
Published: Sep, 1979
Last updated:

Vegetationsperioden i Sverige beräknad från temperaturobservationer.

ReportsMeteorology

 
Type: Report
Report Series: RMK 12
Author: Eriksson, B.
Published: 1978
Last updated:

Temperaturfluktuationer under senaste 100 åren.

ReportsMeteorology

 
Type: Report
Report Series: RMK 14
Author: Eriksson, B.
Published: 1979
Last updated:

SEA ICE AND SNOW INFORMATION FROM DIGITAL PROCESSED SATELLITE DATA - A FEASIBILITY STUDY

ReportsMeteorologyClimate

Computer programs have been developed for handling of NOAA VHRR digital data. The programs include geometric corrections, presentation of calibration data, derivation of data, variation of grey scales, different presentation forms etc. A SAAB D23 computer has been used for the computations. Line …

 
Type: Report
Report Series: RMK 15
Author: Udin, I., och Mattisson, I.
Published: Sep, 1979
Last updated:

Statistiscal analysis of precipitation. Part I. Area precipitation data.

ReportsMeteorologyClimate

Precipitation data on mean values for large areas have been analysed from two points of view. In the first section of this report the data have been looked upon as time series. In the second section they have been regarded as samples from a population.

The reliability of the data is discussed. It …

 
Type: Report
Report Series: RMK 16
Author: Eriksson, B.
Published: Sep, 1979
Last updated:

Statistical Analysis of Precipitation Data Part II Frequency Analysis of Monthly Precipitation Data

ReportsMeteorologyClimate

The frequency distributions of monthly precipitation amounts have been investigated. Data from the period 1931-78 for 262 Swedish and 26 Norwegian stations have been used. The statistical analysis consists of determining the capacity of well-known frequency distribution functions to match the …

 
Type: Report
Report Series: RMK 17
Author: Eriksson, B.
Published: Sep, 1980
Last updated: