Atlantic ocean zones that are quasi-stationary in terms of surface temperature dynamics based on satellite monitoring results

Бесплатный доступ

Using data from the MODIS-Aqua satellite scanner, seasonal changes in ocean surface temperature (OST) in the Atlantic Ocean for the period 2003-2019 were studied. Based on these data, quasi-stationary zones were calculated based on the average monthly ocean surface temperature using the moving window variance method. Zones were identified that are quasi-stationary in terms of the seasonal dynamics of OST and that correspond to the present position of current boundaries. Significant differences in ocean surface temperatures were revealed. Areas in the ocean were identified that differ in absolute OST values, but have similar seasonal dynamics, as well as areas with different seasonal OST dynamics. An interesting fact has been revealed when currents that geographically continue each other do not always coincide in seasonal dynamics. For example, at the boundary of the North Atlantic Current and the Gulf Stream, there is a vast zone with no stable seasonal dynamics. The possibility of using this method for monitoring of mixing zones that arise at the boundaries of currents was shown.

Еще

Atlantic оcean, ocean surface temperature (ost), quasi-stationary zones, modis-aqua, seasonal dynamics

Короткий адрес: https://sciup.org/146282833

IDR: 146282833

Список литературы Atlantic ocean zones that are quasi-stationary in terms of surface temperature dynamics based on satellite monitoring results

  • Zhang R., Sutton R., Danabasoglu G., Kwon Y. O., Marsh R., Yeager S. G., Amrhein D. E., Little C. M. A review of the role of the Atlantic Meridional Overturning Circulation in Atlantic Multidecadal Variability and associated climate impacts. Rev. Geophys., 2019, 57, 316-375. DOI: 10.1029/2019RG000644 EDN: UMHNPE
  • Smeed D. A., Josey S. A., Beaulieu C., Johns W. E., Moat B. I., Frajka-Williams E., Rayner D, Meinen C. S., Baringer M. O., Bryden H. L., McCarthy G. D. The North Atlantic Ocean is in a state of reduced overturning. Geophys. Res. Lett., 2018, 45, 1527-1533. DOI: 10.1002/2017GL076350 EDN: SDISLV
  • Kartushinsky A. V. The investigation on the dynamics of frontal zones in the ocean based on the numerical modelling, using the AVHRR satellite data. Adv. Space Res., 2004, 7(33), 1173-1178. EDN: LIKMXP
  • Khodyaev A. V., Shevyrnogov A. P., Vysotskaya G. S., Kozikova O. S. Using Moving Variance Method to Detect Ocean Currents from Space. J. Sib. Fed. Univ. Eng. technol., 2011, 4(2), 179-184. EDN: NMWLLF
  • Shevyrnogov A. P., Vysotskaya G. S., Shevyrnogov E. A. Spatial and temporal anomalies of sea surface temperature in global scale (by space-based data). Adv. Space Res., 2004, 33, 1179-1183. 10.1016/S 0273-1177(03)00369-7. DOI: 10.1016/S0273-1177(03)00369-7 EDN: LIMUIP
  • Shevyrnogov A. P., Vysotskaya G. S., Gitelson J. I. Quasistationary areas of chlorophyll concentration in the world ocean as observed satellite data. Adv. Space Res., 1996, 18(7), 129-132. EDN: LDKYPV
  • https://oceandata.sci.gsfc.nasa.gov/MODIS-Aqua/Mapped/Monthly/9km.
  • https://lagurus-shop.ru/bengelskoe-tecenie-i-ego-vliyanie-na-klimat).
  • Caesar L., Rahmstorf S., Robinson A., Feulner G., Saba V. Observed fingerprint of a weakening Atlantic Ocean overturning circulation. Nature, 2018, 556, 191-196. DOI: 10.1038/s41586-018-0006-5
Еще
Статья научная