在一个以热带季风为主导的国家使用MAKESENS和机器学习技术进行时空空间分析和预测降雨趋势
Md Moniruzzaman Monir1, Md Rokonuzzaman1, Subaran Chandra Sarker2
1Department of Geography and Environmental Science, Begum Rokeya University, Rangpur, Bangladesh.
Scientific reports
|August 25, 2023
概括
孟加拉国的降雨量呈现下降趋势,特别是在季风和干旱季节,影响水资源. 未来的预测表明,从11月到2月的降雨量最小,预计到2030年之前会出现波动.
科学领域:
- 环境科学 环境科学
- 气候学 气候学 气候学
- 水文学的水文学
背景情况:
- 了解降雨变化对于热带季风地区的水资源管理至关重要.
- 孟加拉国是一个以季风为主导的国家,缺乏关于时空空间降雨趋势的全面数据.
- 气候变化的影响需要对降雨模式进行详细的分析,以制定适应战略.
研究的目的:
- 分析孟加拉国从1980年到2020年的时空降雨变化,以季节和月度的尺度进行分析.
- 使用多层感知 (MLP) 神经网络预测未来降雨变化.
- 为了确定观察到的降雨模式变化的驱动因素.
主要方法:
- 使用MAKESENS,Pettitt测试和创新的趋势分析进行时空降雨趋势分析.
- 在ArcGIS中使用逆距离权重模型进行空间模式分析.
- 使用多层感知 (MLP) 神经网络和ECMWF ERA5再分析数据进行降雨预测.
主要成果:
- 年平均降雨量为2432.6毫米,其中7月至8月的降雨量为57.6%.
- 77%的站点显示每月降雨趋势下降;80%的站点显示11月至3月和8月降雨趋势下降.
- 在季风前,季风前和季风后的季节观察到显著的下降趋势,特别是在特定地区.
结论:
- 孟加拉国的降雨模式正在发生变化,主要下降趋势影响了水的可用性.
- 预测的降雨量表明,从11月到2月的干旱条件和到2030年的波动模式.
- 卷积雨量,云层和湿度分歧的变化可能会导致这些观察到的降雨模式的变化.
相关概念视频
Precipitation and Co-precipitation
1.8K
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...
1.8K
Precipitation Processes
485
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...
485
Precipitation Gravimetry
6.7K
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...
6.7K
Steps in Outbreak Investigation
152
In the ever-evolving field of public health, statistical analysis serves as a cornerstone for understanding and managing disease outbreaks. By leveraging various statistical tools, health professionals can predict potential outbreaks, analyze ongoing situations, and devise effective responses to mitigate impact. For that to happen, there are a few possible stages of the analysis:
152
Precipitation Titration: Endpoint Detection Methods
1.8K
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...
1.8K
Prediction Intervals
2.3K
The interval estimate of any variable is known as the prediction interval. It helps decide if a point estimate is dependable.
However, the point estimate is most likely not the exact value of the population parameter, but close to it. After calculating point estimates, we construct interval estimates, called confidence intervals or prediction intervals. This prediction interval comprises a range of values unlike the point estimate and is a better predictor of the observed sample value, y.
However, the point estimate is most likely not the exact value of the population parameter, but close to it. After calculating point estimates, we construct interval estimates, called confidence intervals or prediction intervals. This prediction interval comprises a range of values unlike the point estimate and is a better predictor of the observed sample value, y.
2.3K


