Table 1 Selected high (higher than 0.8) and low (lower than -0.8) Tibetan Plateau amplification (TA) years according to the interannual component of the TA index and their corresponding values

From: Impact of Tibetan plateau warming amplification on the interannual variations in East Asia Summer precipitation

Ā 

Year

TA_IA ( > 0.8)

NiƱo34_IA (MAM)

NPSI_IA ( > 0.8)

High

1978

1.70

āˆ’0.38

1.21

Ā 

1981

1.63

āˆ’1.22

āˆ’0.09

Ā 

1984

0.85

āˆ’1.24

1.14

Ā 

1994

1.07

āˆ’0.43

2.06

Ā 

2006

1.11

āˆ’0.46

0.28

Ā 

2010

0.82

1.65

āˆ’0.46

Ā 

2013

1.96

āˆ’0.42

0.52

Ā 

2016

1.27

0.94

0.33

Ā 

2018

1.79

āˆ’1.86

0.43

Ā 

2022

2.76

āˆ’0.71

2.02

Low

1976

āˆ’1.80

āˆ’0.30

āˆ’2.72

Ā 

1979

āˆ’0.85

0.25

āˆ’0.09

Ā 

1980

āˆ’0.97

0.19

0.15

Ā 

1983

āˆ’1.28

2.05

āˆ’1.48

Ā 

1992

āˆ’1.08

1.46

āˆ’1.15

Ā 

1997

āˆ’1.02

0.48

āˆ’1.98

Ā 

2011

āˆ’0.84

āˆ’0.79

āˆ’0.34

Ā 

2014

āˆ’0.84

āˆ’0.08

āˆ’0.57

Ā 

2015

āˆ’1.95

0.82

āˆ’0.29

Ā 

2019

āˆ’1.68

1.13

āˆ’1.21

  1. Note that high/low ENSO and NPSI_IA years are marked by bold fonts.