Traditional Culture Encyclopedia - Weather forecast - How to make a weather table for grade two

How to make a weather table for grade two

The weather table is made as follows:

Prepare a piece of paper and a pen and draw a form. You can list the date and weather conditions (sunny/cloudy/rainy/snowy, etc.). ), temperature (can be classified by cold/cool/warm/hot, etc. ) Wait for what you want to record.

Observe the weather every day and fill in the corresponding data in the form. At the end of each statistical period, the frequency of all kinds of weather is counted. For example, how many days are sunny, cloudy and rainy this month?

Visualize the data, which can be displayed in histogram or pie chart, which is more convenient for children to understand the proportion and trend of different weather. Children can draw conclusions by analyzing the data, such as what weather appears most frequently and what weather appears less frequently.

Weather refers to the specific state of the atmosphere near the surface in a short period of time. Weather phenomenon refers to various natural phenomena in the atmosphere, that is, the comprehensive expression of the spatial distribution of various meteorological elements in the atmosphere (such as temperature, pressure, humidity, wind, clouds, fog, rain, flash, snow, frost, thunder, hail, haze, etc.). ) in an instant.

The weather process is the change process of weather phenomena with time in a certain area. All kinds of weather systems have certain time and space scales, and they are intertwined and influence each other.

The combination of many weather systems constitutes a large-scale weather situation and hemispheric and even global atmospheric circulation. The weather system is always in the process of rebirth, development and extinction, and there are corresponding weather phenomena in different development stages.

The direct cause of the wind is the uneven distribution of air pressure in the horizontal direction. Wind is comprehensively influenced by different factors such as atmospheric circulation, topography and water area, and its manifestations are various, such as monsoon, local sea-land wind, valley wind and foehn wind. Simply put, wind is the directional movement of air molecules.

To understand the causes of wind, we must first understand two key concepts: air and air pressure. The components of air include nitrogen molecules (accounting for 78% of the total air volume), oxygen molecules (accounting for about 2 1%), water vapor and other trace components. All air molecules are moving at a very fast speed, colliding with each other and anything on the horizon.