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Method for improving areal aridity/humidity simulating effect

A technology of dry humidity and area, which is applied in special data processing applications, instruments, electrical digital data processing, etc. It can solve the problems of poor dry humidity simulation effect and limited application area, and achieve high accuracy, wide application range, and simulation good effect

Inactive Publication Date: 2017-05-31
INST OF GEOGRAPHICAL SCI & NATURAL RESOURCE RES CAS
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Problems solved by technology

[0006] In order to solve the problems that the traditional model estimation method has poor dry humidity simulation effect and limited application area, the present invention discloses a method for improving the regional dry humidity simulation effect. Through the correction of the traditional model, the accuracy of the model estimation method is improved. In particular, based on the FAO56 model, the present invention corrects the radiation item of the model according to my country's measured radiation data, fills in the gaps in the model's net long-wave radiation correction in the past research, and obtains a calculation reference crop evapotranspiration suitable for my country The empirical coefficient of the radiation item, so that the model results can better represent the maximum possible evapotranspiration in my country's specific natural environment, thereby improving the simulation effect of China's dry humidity

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Embodiment Construction

[0045] The method for improving the regional dry humidity simulation effect of the present invention will be explained and illustrated in detail below in conjunction with the accompanying drawings.

[0046] Such as figure 1 As shown, the invention discloses a method for improving the regional dry humidity simulation effect, the method comprises the following steps,

[0047] Step 1. Collect the monthly meteorological data of each station in the study area and the net longwave radiation data R in the study area nl The present invention divides the site into a regression site and a verification site, such as, 70% of the sites evenly distributed in the research area are regression sites, and 30% of the sites evenly distributed in the research area outside the 70% of the regression sites are verification sites .

[0048] In this embodiment, the monthly meteorological data of the stations in the study area are collected for nearly 30 years, and there are 111 stations with a total ...

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Abstract

The invention discloses a method for improving an areal aridity / humidity simulating effect. The method comprises the following steps: collecting monthly meteorological data of each site in a study area and net long wave radiation data in the study area, calculating total radiation simulation values by at least two total radiation correcting methods respectively, comparing all the total radiation simulation values with a total radiation observation value respectively, and judging out the total radiation correcting method with the highest accuracy; calculating net long wave radiation values by different net long wave radiation calculating methods, then judging out the net long wave radiation calculating method with the highest accuracy, and calculating a radiation correcting formula of net radiation; calculating the largest possible evapotranspiration according to the radiation correcting formula, and calculating an aridity / humidity index according to the largest possible evapotranspiration. Compared with the conventional FAO56 model calculation method, the method provided by the invention has the advantages as follows: through modification of the conventional model estimation method, the aridity / humidity simulating effect is improved, the applicable area of the model estimation method is widened and the model estimation method is higher in accuracy and better in reliability.

Description

technical field [0001] The invention relates to the technical field of climate element calculation, and more specifically, the invention is a method for improving the effect of regional dry humidity simulation. Background technique [0002] As one of the components of climate, the wet and dry conditions play an important role in the spatial distribution of the natural environment. The dryness and wetness of the region are characterized by aridity or humidity index. The former is the ratio of the maximum possible evapotranspiration to precipitation, and the latter is the opposite. They are collectively referred to as the Aridity / Humidity index. Among them, the maximum possible evapotranspiration (ET o ) is also called potential evapotranspiration or reference crop evapotranspiration, which is the sum of surface evaporation and vegetation transpiration under the condition of sufficient water. [0003] Traditional ET o There are three main methods of calculation: lysimeter m...

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Application Information

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Patent Type & Authority Applications(China)
IPC IPC(8): G06F17/50
CPCG06F30/20
Inventor 尹云鹤吴绍洪
Owner INST OF GEOGRAPHICAL SCI & NATURAL RESOURCE RES CAS
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