Variations of pre-monsoon season related atmospheric parameters over Kakinada region

被引:0
|
作者
Vishnu, T. R. [1 ]
Kumar, K. S. [2 ]
Ahammad, S. K. H. [2 ]
Kumar, G. N. S. [3 ]
Umakanth, N. [4 ]
Rao, M. C. [5 ]
Krishna, S. [6 ]
机构
[1] Priyadarshini Inst Technol & Sci Women, Dept Elect & Commun Engn, Chintalapudi, India
[2] Koneru Lakshmaiah Educ Fdn, Dept Elect & Commun Engn, Vaddeswaram, India
[3] RK Coll Engn, Dept Mech Engn, Amaravathi, India
[4] Kallam Haranadhareddy Inst Technol, Dept Elect & Commun Engn, Chowdavaram, India
[5] Andhra Loyola Coll, Dept Phys, Vijayawada, India
[6] Dhanekula Inst Engn & Technol, Dept Elect & Commun Engn, Vijayawada, India
来源
JOURNAL OF THE NATIONAL SCIENCE FOUNDATION OF SRI LANKA | 2023年 / 51卷 / 03期
关键词
Convection; pre-monsoon; soil moisture; total precipitable water; THUNDERSTORMS; KOLKATA; INDEXES;
D O I
10.4038/jnsfsr.v51i3.11380
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Pre-monsoon showers occur before the beginning of the rainy season. From the months of March to May, they take place, and can be anything from little drizzles to powerful thunderstorms. March, April and May are known as the pre-monsoon season (PRMS). The precipitation patterns recorded in PRMS are critical because they have an impact on a wide range of crop-related operations across the country. During PRMS, the maximum temperature (TMAX), minimum temperature (TMIN), soil moisture, relative humidity, latent heat, convective available potential energy (CAPE), and total precipitable water (TPW) were analysed at Kakinada region. These variables were collected using daily ERA5 reanalysis data for the PRMS from 1981 to 2021. Studying the convection-related characteristics over the Kakinada station during the PRMS was our goal. During the study period, the five years with the highest PRMS rainfall were 1990, 1995, 2008, 2010 and 2016 and the five years with the lowest rainfall were 1990, 1995, 2008, 2010 and 2016. In the months leading up to the monsoon, the Kakinada station experiences CAPE values between 1000 and 6000 J/kg, while TPW values are between 25 and 60 mm. The PRMS values for CAPE and TPW both show that the prerequisites for moderate to severe convection activity have been fulfilled. TPW, soil moisture, relative humidity, and CAPE parameters during PRMS were well estimated using the ARMA and ARIMA models.
引用
收藏
页码:555 / 569
页数:15
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