在没有气象参数的情况下建立和评估大气水蒸气逆转模型,基于机器学习
Ning Liu1, Yu Shen1, Shuangcheng Zhang1
1College of Geology Engineering and Geomatics, Chang'an University, Xi'an 710054, China.
Sensors (Basel, Switzerland)
|January 25, 2025
概括
一个新的深度学习模型准确地估计了沉式水蒸气 (PWV),而不需要加权平均温度 (Tm). 这种先进的模型提高了准确性,并且与台风等极端天气事件有很强的相关性.
科学领域:
- 大气科学 大气科学
- 地质物理学 地质物理学
- 遥感 遥感 遥感 遥感
背景情况:
- 降水蒸气 (PWV) 对于了解大气中的水含量至关重要.
- 基于地面的GNSS提供高分辨率的PWV,但受到Tm参数准确度的限制.
- 现有的模型通常依赖于加权平均温度 (Tm),影响PWV反转精度.
研究的目的:
- 为PWV反转开发一种新的深度学习模型,消除了对Tm参数的需求.
- 使用GNSS数据提高PWV估计的准确性和可靠性.
- 调查模型在捕捉极端天气事件中的表现.
主要方法:
- 利用了来自香港的17个地面GNSS站和再分析产品的数据.
- 开发了一个用于PWV检索的深度学习模型,不包括Tm参数.
- 对传统方法和无线电探测器数据验证了模型.
- 分析了台风引起的暴雨事件期间的PWV变化.
主要成果:
- 这种新模型比传统的依赖于Tm的模型更准确,BIAS,MAE和RMSE的平均改善率为38%.
- 无线探测器验证证实了该模型的高精度,显示BIAS仅为0.8毫米.
- 该模型的准确性与LSTM相似,但具有更大的普遍性.
- 新型号检索的PWV在台风期间急剧增加,随后下降,与极端降雨有很强的相关性.
结论:
- 开发的深度学习模型为PWV反转提供了更准确,更可靠的方法.
- 该模型有效地捕捉了极端天气事件期间大气水蒸气的动态变化.
- 这种方法为气象监测提供了有价值的工具,并增强了天气预报能力.
相关概念视频
Precipitation Processes
413
The experimental conditions in a gravimetric analysis should be optimized to maximize the particle size and purity of the obtained precipitate. Ideally, the concentration of the precipitating reagent should be low with effective stirring to maintain low relative supersaturation for the growth of large crystals. In homogeneous precipitation, the precipitant is slowly generated by a chemical reaction in the solution to avoid local reagent excesses. For example, urea decomposes gradually to...
413
Variation of Atmospheric Pressure
2.0K
Change in atmospheric pressure with height is particularly interesting. The decrease in atmospheric pressure with increasing altitude is due to the decreasing gravitational force per unit area as we move away from the surface of the earth.
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...
2.0K
Precipitation Gravimetry
5.2K
Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
5.2K
Precipitation and Co-precipitation
1.7K
Precipitation and coprecipitation methods can be used to separate a mixture of ions in a solution. In qualitative inorganic analysis, ions that form sparingly soluble precipitates with the same reagent are separated based on the differences in solubility products. For example, consider the separation of Cu(II) and Fe(II) ions by precipitation as insoluble sulfides. First, copper(II) sulfide is precipitated by the addition of acidic H2S, where the dissociation of H2S is suppressed. Adding H2S...
1.7K
Precipitation Titration: Endpoint Detection Methods
1.6K
In argentometric precipitation titrations, endpoints can be detected visually by the Mohr, Volhard, and Fajans methods. In the Mohr method, adding a soluble chromate indicator gives an initial yellow color to the analyte solution. As the titrant is added, the first excess of silver ions forms a red silver chromate precipitate, marking the endpoint. The solution pH should be maintained at about 8 by adding solid CaCO3.
In the Volhard method, a standard excess of AgNO3 is first added to the...
In the Volhard method, a standard excess of AgNO3 is first added to the...
1.6K
Vapor Pressure of Fluid
957
The vapor pressure of a fluid is a crucial concept in fluid mechanics, influencing phenomena such as boiling and cavitation. Vapor pressure refers to the pressure exerted by a vapor at a state of thermodynamic equilibrium with its corresponding liquid phase at a specific temperature. It represents the tendency of molecules to escape from the fluid surface into the vapor phase.
When a liquid is placed in a closed container with a small air space, and the space is evacuated, vapor molecules will...
When a liquid is placed in a closed container with a small air space, and the space is evacuated, vapor molecules will...
957


