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WATER VAPOR BALANCE OF THE ATMOSPHERE FROM FIVE YEARS OF HEMISPHERIC DATA
WATER VAPOR BALANCE ATMOSPHERE HEMISPHERIC DATA
2009/10/30
The atmospheric balance of water vapor for the northern hemisphere is
investigated through entirely automatic data processing and objective
analysis procedures, in order to assess the potentialities...
THE EFFECT OF WIND ON THE PRECIPITATION DISTRIBUTION OVER A HILLOCK
EFFECT OF WIND PRECIPITATION DISTRIBUTION HILLOCK
2009/10/30
An account is given of precipitation measuremcnts on a hillock carried
out during June-November 1959 by means of a very dense network of
gauges. It was found that the precipitation distribution in t...
THE EARTH'S GASEOUS HYDROSPHERE AS A NATURAL RESOURCE
EARTH'S GASEOUS HYDROSPHERE NATURAL RESOURCE
2009/10/29
Consideration is given to the desirability of regarding the water vapor of
the atmosphere as a resource for the extraction of fresh liquid water by
artificial means. One method for doing this, previ...
POLE-TO-POLE WATER BALANCE FOR THE IGY FROM AEROLOGICAL DATA
POLE-TO-POLE WATER BALANCE IGY AEROLOGICAL DATA
2009/10/29
The present study gives a discussion of the water balance on a planetary
scale during the IGY covering the mean and the seasonal conditions for
the calendar year 1958. The study includes analyses of...
DEVELOPMENT OF A CONCEPTUAL DETERMINISTIC RAINFALL-RUNOFF MODEL
DEVELOPMENT CONCEPTUAL DETERMINISTIC RAINFALL-RUNOFF MODEL
2009/10/29
This progress report outlines the main principles for the development of
a simple conceptual rainfall-runoff model at the Swedish Meteorological
and Hydrological Institute.
The HBV-2 Model is based...
COOLING PROBLEMS IN THERMALLY POLLUTED RECIPIENTS
COOLING PROBLEMS THERMALLY POLLUTED RECIPIENTS
2009/10/29
The extension of the warm water plume in receiving waters used as recipients
for thermal pollution has been studied using a meteorological
approach. For some real cases thc area of cxcess temperatur...
The ratio of leaf area to ground area required for maintaining potential
cvaporation has been studied in a 4-year investigation, and the influence
of leaf area index on the water use and the actual ...
Seasonal Variability in the Pole-to-Pole Water Vapor Balance During the IGY
Seasonal Variability Pole-to-Pole Water Vapor Balance IGY
2009/10/29
A study of the vertically integrated fields of water vapor and its transport on a
planetary scale derived from aerological data taken during the IGY (International
Geophysical Year) is presented. Th...
Experiences with the Use of the Aerological Method in Evaporation Studies in Northwestern Europe
Aerological Method Evaporation Studies Northwestern Europe
2009/10/29
Two different approaches of the aerological method were used for estimating evaporation in northwestern Europe in the period 1969-1970.
Daily operational aerological observations (»the synoptic...
The Watershed Influence on Storm Runoff in Small Norwegian Rivers
Watershed Influence Storm Runoff Small Norwegian Rivers
2009/10/29
A procedure to isolate and investigate the watershed influence on storm
runoff is presented. It offers an opportunity to study also the change in
influence of particular watershed characteristics by...
Exceptional Groundwater Level Fluctuations at the Dutch Island of Schiermonnikoog
Exceptional Groundwater Level Fluctuations Dutch Island Schiermonnikoog
2009/10/28
During a hydrological-meteorological investigation at a former beachplain at
the Dutch island of Schiermonnikoog, groundwater fluctuations were
recorded. Except for daily changes of the groundwate...
Because of the difficulty of data collection, little is known about the climate
and hydrology of high mountain basins. Following the development of an
automatic weather station (AWS) in the 1960s fo...
The Effect on Storm Runoff Response of Seasonal Variations in Contributing Zones in Small Watersheds
Storm Runoff Response Seasonal Variations Contributing Zones
2009/10/28
Storm runoff production by saturation overland flow has been studied in two
small watersheds in south-central Ontario. One is in rural land use and contains
a wetland. The total saturated zone is at...
Areal Intensity-Duration-Frequency Curves for Short Term Rainfall Events in Lund
Areal Intensity-Duration-Frequency Curves Short Term Rainfall Events
2009/10/28
Design Storms, which are usually derived from point intensity-durationfrequency
(i-d-f) relationships, neither reflect the areal variations of the rainfall
pattern nor the dynamics of the moving sto...
Effects of Excess Rainfall Time Distribution on Catchment Area Hydrograph
Excess Rainfall Time Catchment Area Hydrograph
2009/10/27
The effect of triangular excess hyetographs on catchment area runoff process is
investigated, thereby fixing the precipitation time. The approach accounts for
the kinematic wave theory and allows a ...