Abstract

This paper presents the methodology of taking measurements of active surface energy balance components using the Bowen method. It discusses the applied measurement system, an important part of which are HMD 50U/50Y measurement sensors from Vaisala, adapted to work in the field. Their operation is a source of data for determining vertical profiles of temperature and water vapour pressure. These data are used to determine the turbulence components of the energy balance, i.e., sensible and latent heat. Measurements taken during the vegetative season on rape field showed that intensive evaporation occurred in the period until the end of June and that its decrease coincided with the decrease in the value of the degree of plant development determined on the basis of LAI records. In spring, during the period of intensive plant development, the decade sums of evaporation reached 30 mm, after which their quantities fell to the range of 10–15 mm. They became higher only in the periods of precipitation, when the water from the interception was available.

Highlights

  • Human development over the last several hundred years has had a strong impact on environmental changes, with agriculture leading to huge area changes

  • This paper presents the methodology of taking measurements of active surface energy balance components using the Bowen method

  • Measurements taken during the vegetative season on rape field showed that intensive evaporation occurred in the period until the end of June and that its decrease coincided with the decrease in the value of the degree of plant development determined on the basis of Leaf Area Index (LAI) records

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Summary

Introduction

Human development over the last several hundred years has had a strong impact on environmental changes, with agriculture leading to huge area changes. Rape is one of the most-grown plants, with worldwide crops of around 65–70 million tons. It is mainly used for the production of cooking oil, but it is a source of biofuel. Rapeseed is a winter crop, so it uses both the autumn and spring vegetation period, but it matures and dries up relatively quickly, which means that the field is often devoid of vegetation during the summer. It is very unfavourable from the point of view of the environment and agriculture. It was decided to follow the shaping of the components of the heat balance, including the evapotranspiration of rape during the growing season

Active Surface Energy Balance
Research Area
Research Methodology
Methodology for Calculating the Active Surface Energy Balance Components
The Meteorological Conditions during the Course of Research
Findings
Conclusions
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