• KSII Transactions on Internet and Information Systems
    Monthly Online Journal (eISSN: 1976-7277)

The Analysis of Climate Change in Haiyan County

Vol. 14, No. 10, October 31, 2020
10.3837/tiis.2020.10.001, Download Paper (Free):

Abstract

In this paper, the climate change in Haiyan County in recent decades was analyzed in detail with the methods of moving average, Mann-Kendall non-parametric mutation test and wavelet analysis. According to the variation trend of meteorological factors such as temperature, relative humidity, wind speed, pan evaporation and precipitation in recent decades, the climate of Haiyan County has a tendency of drought, which is becoming more and more serious. From the results of the analysis, the sunshine hours and the air temperature in Haiyan County have an obvious upward trend. The average surface temperature has increased by 2.75 ℃ from 1976, and its largest increase occurred in the late 1970s and 1980s. At this stage, the average surface temperature increased by 1.37 ℃. The relative humidity has a decreasing trend that has decreased by 2.75%. From 1976 to the present, there are two quasi-3a cycles and one quasi-6a cycle. The precipitation and evaporation showed the opposite change trend, in which the trend of precipitation fluctuated upward, while the trend of evaporation showed a fluctuating downward tendency, which led to the serious loss of water in the feeding area. The wind direction in Haiyan County are mainly from west to east, and its wind speed has a trend of slight increase.


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Cite this article

[IEEE Style]
W. Yu, H. Zhang, T. Chen, J. Liu and Y. Shen, "The Analysis of Climate Change in Haiyan County," KSII Transactions on Internet and Information Systems, vol. 14, no. 10, pp. 3941-3954, 2020. DOI: 10.3837/tiis.2020.10.001.

[ACM Style]
Wenzheng Yu, Hanxiaoya Zhang, Tianliang Chen, Jing Liu, and Yanbo Shen. 2020. The Analysis of Climate Change in Haiyan County. KSII Transactions on Internet and Information Systems, 14, 10, (2020), 3941-3954. DOI: 10.3837/tiis.2020.10.001.