Figure 3. Variation of decomposed TCO measured in DU against decomposed CMEs mass in billion ton (BT) for Karachi, Lahore, and Quetta stations along with the correlation coefficient (ρ) values in winter (a), spring (b), summer (c) & autumn (d) seasons during 23rd and 24th solar cycle. Negative slopes in each plot exhibit an inverse relationship

From

Seasonal Effect of CMEs Mass on Pakistan’s Stratospheric Region during 23rd and 24th Solar Cycles

Hiba Haq, Saifuddin Jilani

Applied Ecology and Environmental Sciences. 2023, 11(1), 1-7 doi:10.12691/aees-11-1-1