Seasonal and inter-annual variability of sea surface temperature in the North Indian ocean and associated climate change signatures

2015 ◽  
Author(s):  
Debadatta Swain
Keyword(s):  
Climate Change ◽  
Indian Ocean ◽  
Surface Temperature ◽  
Sea Surface Temperature ◽  
North Indian Ocean ◽  
Sea Surface ◽  
Annual Variability ◽  
The North

scholarly journals On the diurnal ranges of Sea Surface Temperature (SST) in the north Indian Ocean

2009 ◽  
Vol 118 (5) ◽  
pp. 483-496 ◽  
Author(s):  
S. S. C. Shenoi ◽  
N. Nasnodkar ◽  
G. Rajesh ◽  
K. Jossia Joseph ◽  
I. Suresh ◽  
...  
Keyword(s):  
Indian Ocean ◽  
Surface Temperature ◽  
Sea Surface Temperature ◽  
North Indian Ocean ◽  
Sea Surface ◽  
The North

scholarly journals Sea surface temperature variability over North Indian Ocean — A study of two contrasting monsoon seasons

1986 ◽  
Vol 95 (3) ◽  
pp. 435-446 ◽  
Author(s):  
M. R. Ramesh Kumar ◽  
S. Sathyendranath ◽  
N. K. Viswambharan ◽  
L. V. Gangadhara Rao
Keyword(s):  
Indian Ocean ◽  
Surface Temperature ◽  
Sea Surface Temperature ◽  
North Indian Ocean ◽  
Temperature Variability ◽  
Sea Surface

Meridional Distribution of Surface CO2 along 67°E of the Indian Ocean

2020 ◽  
Author(s):  
Dong-Jin Kang ◽  
Sang-Hwa Choi ◽  
Daeyeon Kim ◽  
Gyeong-Mok Lee
Keyword(s):  
Indian Ocean ◽  
Surface Temperature ◽  
Sea Surface Temperature ◽  
Sea Surface ◽  
Sea Surface Salinity ◽  
Surface Seawater ◽  
Surface Salinity ◽  
The North ◽  
The Indian Ocean ◽  
North And South

<p>Surface seawater carbon dioxide was observed from 3 °S to 27 °S along 67 °E of the Indian Ocean in April 2018 and 2019. Partial pressure of CO<sub>2</sub>(pCO<sub>2</sub>) in the surface seawater and the atmosphere were observed every two minutes using an underway CO2 measurement system (General Oceanics Model 8050) installed on R/V Isabu. Surface water temperature and salinity were measured as well. The pCO<sub>2</sub> was measured using Li-7000 NDIR. Standard gases were measured every 8 hours in five classes with concentrations of 0 µatm, 202 µatm, 350 µatm, 447 µatm, and 359.87 µatm. The fCO<sub>2</sub> of atmosphere remained nearly constant at 387 ± 2 µatm, but the surface seawater fCO<sub>2</sub> peaked at about 3 °S and tended to decrease toward the north and south. The distribution of fCO<sub>2</sub> in surface seawater according to latitude tends to be very similar to that of sea surface temperature. In order to investigate the factors that control the distribution of fCO<sub>2</sub> in surface seawater, we analyzed the sea surface temperature, sea surface salinity, and other factors. The effects of salinity are insignificant, and the surface fCO<sub>2</sub> distribution is mainly controlled by sea surface temperature and other factors that can be represented mainly by biological activity and mixing.</p>

scholarly journals The role of local sea surface temperature pattern changes in shaping climate change in the North Atlantic sector

2018 ◽  
Vol 52 (1-2) ◽  
pp. 417-438 ◽  
Author(s):  
Ralf Hand ◽  
Noel S. Keenlyside ◽  
Nour-Eddine Omrani ◽  
Jürgen Bader ◽  
Richard J. Greatbatch
Keyword(s):  
Climate Change ◽  
Surface Temperature ◽  
Sea Surface Temperature ◽  
North Atlantic ◽  
Sea Surface ◽  
Temperature Pattern ◽  
Atlantic Sector ◽  
The North ◽  
The North Atlantic
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