地球科学と気候変動ジャーナル

抽象的な

Influence of Pacific and Indian Ocean Temperatures on Monsoonal Rainfall in India

Abdul Rehman, Mohammad Sharif, Mohammad Shakeel

PDO is a strong, recurring shape of the ocean surroundings in climate change variability central along mid-latitude in Pacific Ocean basin. The large climate change indices like PDO (Pacific Decadal Oscillation) and IOD (Indian Ocean Dipole) presence and their relationships for the hydrologic ways on surface response is an important scale of influences on maximum values of precipitation. PDO have particular implications for world climate changing Pacific dry spell and the flooding is under Pacific Ocean basin, the efficiency of sea ecosystems, and world surface temperature models. So, the main purposes of this research were to analyse the relationships of PDO and monsoonal rainfall at all 40 meteorological rainfall stations across the country. The present study focuses on the investigation in linking the point rainfall with ENSO than conventional method of average precipitation in the big region. The results presented a negative connection PDO index versus rainy season precipitation at most of rainfall stations take into consideration for this research. Six rainfall stations such as, Hissar, Gaya, Kolkata, Guwahati, Mysore and Bhubaneswar show a correlation that is positive between PDO and monsoonal rainfall in India. It is established that based on analysis of relationships of with rainy season precipitation at various rainfall stations that a PDO is correlated along imperfect Indian storm. The high level in comprehension the relationships of huge scale indices such as PDO and IOD with terrain hydrologic actions have ability to improve Indian monsoon season forecasting capability across the India.