Role of Natural and Anthropogenic Loadings on Indian Temperature Trends
We evaluate the impact of natural and anthropogenic loadings on Indian maximum ( T max ) and minimum ( T min ) temperature variabilities during 1901–2015 using multiple spectral and statistical analyses. We compare the significant eigenmodes of temperature with TSI, Ocean and Atmospheric Processes (...
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Published in | Pure and applied geophysics Vol. 176; no. 11; pp. 5125 - 5140 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Cham
Springer International Publishing
01.11.2019
Springer Nature B.V |
Subjects | |
Online Access | Get full text |
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Summary: | We evaluate the impact of natural and anthropogenic loadings on Indian maximum (
T
max
) and minimum (
T
min
) temperature variabilities during 1901–2015 using multiple spectral and statistical analyses. We compare the significant eigenmodes of temperature with TSI, Ocean and Atmospheric Processes (OAP) such as ENSO, PDO, NAO, AMO and CO
2
data to understand their influence on temperature. The present analysis is based on new eigen-weighted correlation coefficient (EWCC) and regression analysis to assess the sensitivity of temperature to TSI, OAP and CO
2
. The first eigenmodes (EM) of
T
max
and
T
min
representing the long-term trend correlate well with the first EM of TSI (EWCC: 0.90 and 0.78) and CO
2
(EWCC: 0.95 and 0.72), respectively. The CO
2
residing throughout the day and night in the atmosphere may produce a similar linearly increasing trend in
T
max
and
T
min
. However, the trend test revealed non-stationarity in the trends of
T
max
and
T
min
. In addition, the regression analysis revealed high sensitivity of the
T
max
and
T
min
trend to TSI compared with CO
2
. Our study suggests that there is an intermittent change in the running mean of TSI between 1901 and 2015 resulting in observed changes in
T
max
. In addition, spectral analysis of the
T
max
and
T
min
records revealed statistical significant periodicities of ~ 2–7 years and 11 ± 2 years in
T
max
and ~ 2–7 years and 50 ± 4 years in
T
min
, which may be associated with OAP and TSI, respectively. Based on the present analyses, we conclude that there are combined responses of (1) intrinsic variation in TSI and CO
2
, which may be interpreted as the major loading factors on the trend of
T
max
and
T
min
, respectively; (2) periodic variabilities in different frequency bands may be associated with both solar and ocean atmospheric processes depending upon time scales. |
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ISSN: | 0033-4553 1420-9136 |
DOI: | 10.1007/s00024-019-02247-8 |