Loading…

Trends and Anomalies in Extreme Climate Indices and Influence of El Niño and La Niña over Pranhita Catchment in Godavari Basin, India

AbstractHydrologic design and planning requires dealing with extremes in precipitation and temperature events caused due to climate change. Long-term trends and variability in 20 extreme climate indices (ECIs) and the influence of El Niño and La Niña over the Pranhita catchment, India are studied fo...

Full description

Saved in:
Bibliographic Details
Published in:Journal of hydrologic engineering 2016-02, Vol.21 (2)
Main Authors: Bothale, Rajashree Vinod, Katpatal, Yashwant B
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:AbstractHydrologic design and planning requires dealing with extremes in precipitation and temperature events caused due to climate change. Long-term trends and variability in 20 extreme climate indices (ECIs) and the influence of El Niño and La Niña over the Pranhita catchment, India are studied for the period of 1951–2013. An overall increase in daily precipitation, more intense rain, and an increase in continuous dry days are observed; however, total rain shows a negative trend. A warming trend is observed with an increase in dry days, warm days, and hot nights, and a decrease in the frequency of cool days and nights. Observed +ve trends for maximum and minimum temperatures are 0.7 and 0.8°C, respectively. El Niño years resulted in −ve anomaly and +ve anomaly was observed during La Niña years for the majority of ECIs. The association between ENSO and yearly temperature indices is found to be weak in comparison with precipitation indices. The study confirmed the multimodal nature of precipitation during El Niño, high precipitation during La Niña, and excess postmonsoon rains during La Niña. A comparison between the Oceanic Nino Index (ONI) and the precipitation anomaly showed that the anomaly changes with a phase change in ENSO with the relation being very prominent during El Niño. The El Niño years have resulted in a precipitation deficit, and the La Niña years have resulted in excess precipitation.
ISSN:1084-0699
1943-5584
DOI:10.1061/(ASCE)HE.1943-5584.0001283