guhan velusamy

Mr. guhan velusamy


Research Focus & Metrics

Academic Career Length

7Years (2020-Present)

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

Representative Publications

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8 April 2024 in Scientific Reports
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Journal Article
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GVguhan velusamy
guhan velusamy
KAK. Annadurai
K. Annadurai
SES. Easwaran
S. Easwaran
MMM. Marimuthu
M. Marimuthu
DBD. Balu
D. Balu
CNC. Navinkumar
C. Navinkumar
The DSSAT CANEGRO model was calibrated and verified using field experimental data from five Tamil Nadu Agroclimatic Zones (1981–2022). The genetic coefficients of the sugarcane cultivar (CO-86032) were calculated. R2 obtained between measured and simulated stalk fresh mass was 0.9 with the nRMSE (0.01) and RMSE (1.6) and R2 between measured and simulated sucrose mass was 0.9 with the nRMSE (0.16) and RMSE (1.2). For yield R2 obtained between measured and simulated was 0.9 with the nRMSE (0.01) and RMSE (1.6). As a result, the CANEGRO model may be used to mimic the phenology and yield features of the sugarcane cultivar in Tamil Nadu's Agro Climatic Zones. Temperature increases in Agro Climatic Zones resulted in varying yield reductions, with 2 °C increases causing a 3% loss, 3 °C increases 5%, and 4 °C increases 9%. The Water Requirement rose throughout all of the ACZ due to the high temperature, but to differing degrees. A 2 °C increase often results in an average 4% increase in the WR. 3 °C rise in temperature increased WR to 9% and WR rose by 13% when the temperature was raised by 4 °C.

22 July 2025 in Journal of Atmospheric and Solar-Terrestrial Physics
Verified
Journal Article
Closed access
GVguhan velusamy
guhan velusamy
ARA. Dharma Raju
A. Dharma Raju
KKK. Rama Krishna
K. Rama Krishna
KNK. Nagaratna
K. Nagaratna

25 December 2025 in International Journal of Climatology
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Journal Article
Closed access
GVguhan velusamy
guhan velusamy
DADharma Raju Akasapu
Dharma Raju Akasapu
NKNagaratna Kopparthi
Nagaratna Kopparthi

27 October 2020 in International Journal of Environment and Climate Change
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GVguhan velusamy
guhan velusamy
VGV. Geethalakshmi
V. Geethalakshmi
KBK. Bhuvaneswari
K. Bhuvaneswari
MRM. Rajavel
M. Rajavel
DPDhanya Praveen
Dhanya Praveen
KSK. Senthilraja
K. Senthilraja
Rainfall is one of the most important climatic variables that determine the spatial and temporal patterns of climate variability of a region, which also provides useful information for the planning of water resources, agricultural production, and others. Climate change is one of the most significant worldwide issues talked among scientists and researchers, and one of the consequences of climate change is the alteration of rainfall patterns. 'India's population and the economy is linked to climate-sensitive activities, including rainfed agriculture and excess climate anomalies, deficient and flooded rainfall years have a dramatic impact on the economy as well as on the living conditions of the inhabitants of the affected region. An understanding of current and historical trends and variation is inevitable to her future development, especially in agricultural and hydrological sectors. In the present study, historical weather data for 33 years (1981-2013) was analyzed for rainfed cropping season (September - December) to understand the climatic variability in the Kanyakumari district of Tamil Nadu. The maximum daily air temperature increased on average by 0.02°C per year, whereas minimum daily air temperature remained constant during the rainfed cropping season. The high rainfall zone receives an annual and rainfed cropping average rainfall of 1307and 672 mm, respectively. Analysis of rainfall during rainfed cropping period over 33 years showed ten years had standard RF, nine years had deficit rainfall, six years had below standard RF, one year had above standard RF and seven years had excess RF. Analysis indicates that the deficit condition prevailed in every alternate year in recent decades. The onset of rainfed cropping season varied over the years (1981-2013), 13 years had onset in the slot from 1st to 5th  September, and in others, years onset occurred between 6 and 30th September. Cessation also had a variation over 33 years and 16 years had cessation from 26 to 31st December while remaining years had cessation in the period of 1-25th December. LGP ranged from 57 to 143 days, with an average LGP of 106 days. Dry spell varied from 3 to 12 days with the mean of 6 days, and wet spell varied from 2 to 8 days with an average of 5 days.

9 October 2025 in Aerosol Science and Engineering
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GVguhan velusamy
guhan velusamy
DADharma Raju Akasapu
Dharma Raju Akasapu
NKnaga ratna Kopparthi
naga ratna Kopparthi
KCKavitha Chandu
Kavitha Chandu

1 January 2024 in Madras Agricultural Journal
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GVguhan velusamy
guhan velusamy
SASravani A
Sravani A
RVRao L V
Rao L V
MAMurali Krishna A
Murali Krishna A
MBMuralidhar B
Muralidhar B
This research uses the Markov Chain Model to analyze dry and wet spells in Telangana, India’s Adilabad district. The research intends to provide significant insights for agricultural planning in the region, which is critical considering that agriculture is the foundation of Indian economy. The study emphasizes the need to understand and effectively exploit natural resources, particularly rainfall, for the improvement and sustainability of rainfed agriculture. According to the calculation, there is a 70% chance of two consecutive wet weeks throughout the monsoon season (24th SMW to 40th SMW), resulting in about 17 weeks of monsoon rain in the Adilabad area. This enables the successful development of short-duration crops like rice. According to the study, the Markov Chain Model is effective for simulating the long-term frequency behavior of wet or dry spells, providing a comprehensive understanding of rainfall patterns and their impact on agriculture in the Adilabad District