Solar control on the cloud liquid water content and integrated water vapor associated with monsoon rainfall over India

被引:11
作者
Maitra, Animesh [1 ]
Saha, Upal [1 ]
Adhikari, Arpita [1 ]
机构
[1] Univ Calcutta, Inst Radio Phys & Elect, Kolkata 700009, India
关键词
Solar activity; Galactic Cosmic Ray; Liquid water content; Integrated water vapor; Monsoon rainfall; Wavelet analysis; SUMMER MONSOON; COSMIC-RAYS; CLIMATE; VARIABILITY; CYCLE; FREQUENCY; AEROSOLS;
D O I
10.1016/j.jastp.2014.06.010
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
A long-term observation over three solar cycles indicates a perceptible influence of solar activity on rainfall and associated parameters in the Indian region. This paper attempts to reveal the solar control on the cloud liquid water content (LWC) and integrated water vapor (IWV) along with Indian Summer Monsoon (ISM) rainfall during the period of 1977-2012 over nine different Indian stations. Cloud LWC and IWV are positively correlated with each other. An anti-correlation is observed between the Sunspot Number (SSN) and ISM rainfall for a majority of the stations and a poor positive correlation obtained for other locations. Cloud LWC and IWV possess positive correlations with Galactic Cosmic Rays (GCR) and SSN respectively for most of the stations. The wavelet analyses of SSN, ISM rainfall, cloud LWC and IWV have been performed to investigate the periodic characteristics of climatic parameters and also to indicate the varying relationship of solar activity with ISM rainfall, cloud LWC and IWV. SSN, ISM rainfall and IWV are found to have a peak at around 10.3 years whereas a dip is observed at that particular period for cloud LWC. (C) 2014 Elsevier Ltd. All rights reserved.
引用
收藏
页码:157 / 167
页数:11
相关论文
共 50 条
  • [1] The effect of 10.7 cm solar flux on the monsoon rainfall over India
    Midya, S. K.
    Goswami, S.
    Sengupta, K.
    JOURNAL OF INDIAN GEOPHYSICAL UNION, 2016, 20 (06): : 558 - 565
  • [2] Rainfall estimation from liquid water content and precipitable water content data over land, ocean and plateau
    Chakraborty, S.
    Adhikari, A.
    Maitra, A.
    ATMOSPHERIC RESEARCH, 2016, 167 : 265 - 274
  • [3] Spatial Coherence of Water Vapor and Rainfall over the Indian Subcontinent during Different Monsoon Seasons
    Radhakrishna, Basivi
    Rao, T. Narayana
    Saikranthi, K.
    JOURNAL OF HYDROMETEOROLOGY, 2019, 20 (01) : 45 - 58
  • [4] An Observational Study of GPS-Derived Integrated Water Vapor over India
    Gopalan, Kaushik
    Shukla, Bipasha Paul
    Sharma, Som
    Kumar, Prashant
    Shyam, Abhineet
    Gaur, Amita
    Sunda, Surendra
    ATMOSPHERE, 2021, 12 (10)
  • [5] Modulation of Indian monsoon by water vapor and cloud feedback over the past 22,000 years
    Jalihal, Chetankumar
    Srinivasan, Jayaraman
    Chakraborty, Arindam
    NATURE COMMUNICATIONS, 2019, 10 (1)
  • [6] Roles of water vapor sources and transport in the intraseasonal and interannual variation in the peak monsoon rainfall over East China
    Chu, Qucheng
    Wang, Qiguang
    Feng, Guolin
    Jia, Zikang
    Liu, Gang
    CLIMATE DYNAMICS, 2021, 57 (7-8) : 2153 - 2170
  • [7] Analysis of Precipitable Water Vapor, Liquid Water Path and Their Variations before Rainfall Event over Northeastern Tibetan Plateau
    Xue, Mingxing
    Li, Qiong
    Qiao, Zhen
    Zhu, Xiaomei
    Tysa, Suonam Kealdrup
    ATMOSPHERE, 2024, 15 (08)
  • [8] Atmospheric Water Vapor Transport Associated with Two Decadal Rainfall Shifts over East China
    Li, Xiuzhen
    Wen, Zhiping
    Zhou, Wen
    Wang, Dongxiao
    JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN, 2012, 90 (05) : 587 - 602
  • [9] Principal Components Analysis of Rainfall and Associated Synoptic Models of the Southwest Monsoon over India
    U. S. De
    A. B. Mazumdar
    Theoretical and Applied Climatology, 1999, 64 : 213 - 228
  • [10] Principal components analysis of rainfall and associated synoptic models of the southwest monsoon over India
    De, US
    Mazumdar, AB
    THEORETICAL AND APPLIED CLIMATOLOGY, 1999, 64 (3-4) : 213 - 228