hydrophysicsФундаментальная и прикладная гидрофизикаFundamental and Applied Hydrophysics2073-66732782-5221St. Petersburg Research Center of the Russian Academy of Sciences10.7868/S2073667321040067hydrophysics-133Research ArticleГИДРОФИЗИЧЕСКИЕ И БИОГЕОХИМИЧЕСКИЕ ПОЛЯ И ПРОЦЕССЫHYDROPHYSICAL AND BIOGEOCHEMICAL FIELDS AND PROCESSESВлияние обратной связи температура воды–фитопланктон на температуру верхнего слоя Индийского океанаInfluence of the water temperature–phytoplankton feedback on the upper layer temperature of the Indian OceanСеинД. В.SeinD. V.

117997, Нахимовский пр., д. 36, г. Москва

27570, Бремерхафен, Ам Хандельсхафен 12, Германия 

117997, Nahimovskiy prospekt, 36, Moscow

27570, Am Handelshafen 12, Bremerhaven, Germany

dmitry.sein@awi.deДворниковА. Ю.DvornikovA. Yu.

117997, Нахимовский пр., д. 36, г. Москва

117997, Nahimovskiy prospekt, 36, Moscow

МартьяновС. Д.MartyanovS. D.

117997, Нахимовский пр., д. 36, г. Москва

117997, Nahimovskiy prospekt, 36, Moscow

КабосУ.CabosW.

28801, Алькала де Энарес, Площадь Сан-Диего, Мадрид

28801, Alcalf de Henares, Square San Diego, Alcala

РябченкоВ. А.RyabchenkoV. A.

117997, Нахимовский пр., д. 36, г. Москва

117997, Nahimovskiy prospekt, 36, Moscow

ГрёгерМ.GrögerM.

D-18119, Варнемюнде, Зеештрассе 15, Росток

D-18119, Seestrasse 15, Warnemünde, Rostock

МишраА. К.MishraA. K.

462066, Бхопал Байпасс Роад, Бхаури, Бхопал, Мадхья Прадеш

462066, Bhopal Bypass Road, Bhauri, Bhopal, Madhya Pradesh Bhopal

КумарП.KumarP.

462066, Бхопал Байпасс Роад, Бхаури, Бхопал, Мадхья Прадеш

462066, Bhopal Bypass Road, Bhauri, Bhopal, Madhya Pradesh Bhopal

ГорчаковВ. А.GorchakovV. A.

117997, Нахимовский пр., д. 36, г. Москва

117997, Nahimovskiy prospekt, 36, Moscow

Институт океанологии им. П.П. Ширшова РАН; Институт Альфреда Вегенера, Центр полярных и морских исследований имени ГельмгольцаРоссияShirshov Institute of Oceanology, Russian Academy of Sciences; Alfred Wegener Institute, Helmholtz Centre for Polar and Marine ResearchRussian FederationИнститут океанологии им. П.П. Ширшова РАНРоссияShirshov Institute of Oceanology, Russian Academy of SciencesRussian FederationУниверситет АлькалыИспанияUniversity of AlcalaSpainИнститут исследований Балтийского моря им. ЛейбницаГерманияLeibniz Institute for Baltic Sea ResearchGermanyДепартамент наук о Земле и окружающей среде, Индийский институт естественнонаучного образования и исследованийИндияDepartment of Earth and Environmental Sciences, Indian Institute of Science Education and ResearchIndia2021141220211446476Copyright © Сеин Д.В., Дворников А.Ю., Мартьянов С.Д., Кабос У., Рябченко В.А., Грёгер М., Мишра А.К., Кумар П., Горчаков В.А., 20212021Сеин Д.В., Дворников А.Ю., Мартьянов С.Д., Кабос У., Рябченко В.А., Грёгер М., Мишра А.К., Кумар П., Горчаков В.А.Sein D.V., Dvornikov A.Y., Martyanov S.D., Cabos W., Ryabchenko V.A., Gröger M., Mishra A.K., Kumar P., Gorchakov V.A.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://hydrophysics.spbrc.ru/jour/article/view/133

В результате экспериментов с региональной климатической моделью системы Земли обнаружено, что в эксперименте, в котором ослабление света рассчитывается с учетом обратной связи между температурой воды и фитопланктоном, средняя температура поверхности моря ниже на большей части Индийского океана в тропиках по сравнению с эталонным экспериментом, в котором используется постоянный коэффициент ослабления света (равный 0.06 м–1), типичный для глобальных расчетов с климатической моделью системы Земли. Установлено также, что наиболее сильные различия (более 1 °C) в температуре поверхности моря наблюдаются в летний период. В эксперименте с учетом указанной обратной связи отмечается также охлаждение приповерхностных слоев океана и смещение термоклина вверх. Последнее, а также сезонные изменения коэффициента ослабления света заметно приближают модельные результаты к данным наблюдений. Таким образом, включение полной обратной связи между температурой воды и фитопланктоном с соответствующим коэффициентом ослабления света в целом понижает температуру поверхности моря и температуру воды в подповерхностных слоях тропической части Индийского океана, что имеет серьезные последствия для взаимодействия океана и атмосферы и, следовательно, для моделирования регионального климата.

Two experiments with a regional Earth System Model (ESM) are performed. We discovered that in a simulation where light attenuation is calculated taking into account the water temperature–phytoplankton feedback the average sea surface temperature (SST) is lower over most of the tropical Indian ocean in comparison with the reference experiment in which a constant light attenuation coefficient equal to 0.06 m-1, typical in global ESM runs, is used. We also find that the strongest differences (more than 1 °C) in SST occur in the summer period and a cooling of subsurface layers and a rise of the thermocline are noted in the experiment with the above feedback. Thus, including the full water temperature–phytoplankton feedback with corresponding light attenuation coefficient generally lowers the SST and water temperature in subsurface layers of the Indian ocean, with strong implications for the ocean-atmosphere coupling and, therefore for the simulated regional climate.

температура водыфитопланктонослабление светаклиматическая модель системы ЗемлиИндийский океанwater temperaturephytoplanktonlight attenuationEarth System ModelIndian OceanРабота финансируется совместно Российским научным фондом (RSF), проект № 19–47–02015, и Департаментом науки и технологий (DST) Правительства Индии (грант № DST/INT/RUS/RSF/P-33/G) в рамках проекта «Влияние изменений климата на экстремальные явления в Южной Азии: оценки на основе региональной климатической модели земной системы высокого разрешения». Исследование выполнено в рамках государственного задания Минобрнауки России (№ 0128–2021–0014). В работе использовались ресурсы Немецкого центра климатических вычислений (DKRZ), предоставленные его Научным руководящим комитетом (WLA) в рамках проекта с идентификатором ba1144.ReferencesSzabo S. et al. Making SDGs work for climate change hotspots // Environment: Science and Policy for Sustainable Development. 2016. V. 58, N 6. 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The authors declare that there are no conflicts of interest present.