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Evaporation | Web Scraping Tool | ScrapeStorm

2025-11-26 15:10:33

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Abstract：Evaporation refers to the total amount of water that enters the atmosphere from the Earth's surface (water bodies, soil, vegetation, etc.) through evaporation within a certain period of time (such as day, month, year). It is usually measured in millimeters (mm) and is measured using tools such as evaporation pans, weather stations, or remote sensing satellites. It is an important indicator reflecting the regional water cycle, drought level, and water resource sustainability. ScrapeStormFree Download

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Introduction

Evaporation refers to the total amount of water that enters the atmosphere from the Earth’s surface (water bodies, soil, vegetation, etc.) through evaporation within a certain period of time (such as day, month, year). It is usually measured in millimeters (mm) and is measured using tools such as evaporation pans, weather stations, or remote sensing satellites. It is an important indicator reflecting the regional water cycle, drought level, and water resource sustainability.

Applicable Scene

Evaporation data is applicable to fields such as agricultural irrigation scheduling, water resource management, climate research, and ecological protection, providing key data support for assessing drought risk, optimizing water use efficiency, and developing disaster prevention and mitigation strategies.

Pros: Evaporation, by quantifying the rate of water loss, provides precise data for agricultural irrigation, water resource planning, and climate research, effectively guiding the formulation of water-saving measures and drought early warning, and contributing to regional sustainable development.

Cons: Evaporation is significantly affected by meteorological conditions, surface characteristics, and measurement methods. The data fluctuates greatly and has limited spatial representativeness. It needs to be combined with other indicators for comprehensive analysis to accurately reflect the actual water dynamics.