Karuppasamy Ponnambalam Manikandan

Dr. Karuppasamy Ponnambalam Manikandan

orcid

Research Focus & Metrics

Academic Career Length

13Years (2014-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 October 2016 in Science of The Total Environment
Verified
Journal Article
Closed access
PKPeriyadan K. Krishnakumar
Periyadan K. Krishnakumar
MQMohammad A. Qurban
Mohammad A. Qurban
MSMichael Stiboller
Michael Stiboller
KNKeeve E. Nachman
Keeve E. Nachman
TJThadickal Joydas
Thadickal Joydas
KFKevin A. Francesconi
Kevin A. Francesconi

1 July 2019 in Ecological Indicators
Verified
Journal Article
Closed access
Wenzhao LiWenzhao Li
Wenzhao Li
Hesham ElaskaryHesham Elaskary
Hesham Elaskary
MQMohamed A. Qurban
Mohamed A. Qurban
JLJingjing Li
Jingjing Li
KMKaruppasamy Ponnambalam Manikandan
Karuppasamy Ponnambalam Manikandan
TPThomas Piechota
Thomas Piechota

26 April 2018 in Remote Sensing
Verified
Journal Article
Open access
PDF file
Wenzhao LiWenzhao Li
Wenzhao Li
Hesham ElaskaryHesham Elaskary
Hesham Elaskary
MQMohammed Qurban
Mohammed Qurban
EPEmmanouil Proestakis
Emmanouil Proestakis
MGMichael Garay
Michael Garay
KMKaruppasamy Ponnambalam Manikandan
Karuppasamy Ponnambalam Manikandan
This study considers the various factors that regulate nutrients supply in the Red Sea. Multi-sensor observation and reanalysis datasets are used to examine the relationships among dust deposition, sea surface temperature (SST), and wind speed, as they may contribute to anomalous phytoplankton blooms, through time-series and correlation analyses. A positive correlation was found at 0–3 months lag between chlorophyll-a (Chl-a) anomalies and dust anomalies over the Red Sea regions. Dust deposition process was further examined with dust aerosols’ vertical distribution using satellite lidar data. Conversely, a negative correlation was found at 0–3 months lag between SST anomalies and Chl-a that was particularly strong in the southern Red Sea during summertime. The negative relationship between SST and phytoplankton is also evident in the continuously low levels of Chl-a during 2015 to 2016, which were the warmest years in the region on record. The overall positive correlation between wind speed and Chl-a relate to the nutritious water supply from the Gulf of Aden to the southern Red Sea and the vertical mixing encountered in the northern part. Ocean Color Climate Change Initiative (OC-CCI) dataset experience some temporal inconsistencies due to the inclusion of different datasets. We addressed those issues in our analysis with a valid interpretation of these complex relationships.

1 April 2016 in Journal of Marine Systems
Verified
Journal Article
Closed access
MWMohideen Wafar
Mohideen Wafar
MQMohammad Ali Qurban
Mohammad Ali Qurban
MAMohamed Ashraf
Mohamed Ashraf
KMKaruppasamy Ponnambalam Manikandan
Karuppasamy Ponnambalam Manikandan
AFAce Vincent Flandez
Ace Vincent Flandez
ABArvin C. Balala
Arvin C. Balala

1 July 2014 in Deep Sea Research Part I: Oceanographic Research Papers
Verified
Journal Article
Closed access
MQMohammad A. Qurban
Mohammad A. Qurban
PKP.K. Krishnakumar
P.K. Krishnakumar
TJThadickal Joydas
Thadickal Joydas
KMKaruppasamy Ponnambalam Manikandan
Karuppasamy Ponnambalam Manikandan
TAT.T.M. Ashraf
T.T.M. Ashraf
SCS.D. Cairns
S.D. Cairns

1 May 2015 in Journal of Sea Research
Verified
Journal Article
Closed access
TJThadickal Joydas
Thadickal Joydas
MQMohammad A. Qurban
Mohammad A. Qurban
KMKaruppasamy Ponnambalam Manikandan
Karuppasamy Ponnambalam Manikandan
TAT.T.M. Ashraf
T.T.M. Ashraf
SAS.M. Ali
S.M. Ali
PKP.K. Krishnakumar
P.K. Krishnakumar