Heat content and temperature trends in the Mediterranean Sea as derived from Argo float data

被引:3
|
作者
Kubin, Elisabeth [1 ]
Menna, Milena [1 ]
Mauri, Elena [1 ]
Notarstefano, Giulio [1 ]
Mieruch, Sebastian [2 ]
Poulain, Pierre-Marie [1 ]
机构
[1] Inst Oceanog & Appl Geophys, Sect Oceanog, Trieste, Italy
[2] Alfred Wegener Inst, Sect Marine Geol, Bremerhaven, Germany
关键词
heat content trends; temperature trends; Argo floats; Mediterranean Sea; Mediterranean sub-basins; dense water formation areas; climate change; DENSE WATER FORMATION; OSCILLATING SYSTEM BIOS; ADRIATIC SEA; DECADAL VARIABILITY; MARINE HEATWAVES; CLIMATE-CHANGE; IONIAN SEAS; AEGEAN SEA; ENERGY; CIRCULATION;
D O I
10.3389/fmars.2023.1271638
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Mediterranean Sea is very sensitive to climatic changes due to its semi-enclosed nature and is therefore defined as one of the hotspots in future climate change projections. In this study, we use Argo float data to assess climatologies and trends in temperature and Ocean Heat Content (OHC) throughout the Mediterranean Sea and for specific sub-basins (e.g. Western and Eastern Mediterranean, Gulf of Lion, South Adriatic). The amount of the OHC, spatially averaged in bins of 1 degrees x1 degrees over the period from 2001 to 2020, increases from west to east in the Mediterranean Sea. Time series of temperature and OHC from 2005 to 2020, estimated in the surface and intermediate layers (5-700 m) and deeper layer (700-2000 m), reveal significant warming trends and an increase of OHC. The upper 700 m of the Mediterranean Sea show a temperature trend of 0.041 +/- 0.012 degrees C center dot yr-1, corresponding to an annual increase in OHC of 3.59 +/- 1.02 W center dot m-2. The Western Mediterranean Sea (5-700 m) is warming fastest with an increase in temperature at a rate of 0.070 +/- 0.015 degrees C center dot yr-1, corresponding to a yearly increase in OHC of 5.72 +/- 1.28 W center dot m-2. Mixing and convection events within convection sites and along boundary currents transport and disperse the temperature and OHC changes. Significant warming trends are evident in the deeper layers (700-2000 m) of the two deep convection sites in the Mediterranean Sea (Gulf of Lion, South Adriatic), with an exceptionally strong warming trend in the South Adriatic from 2013 to 2020 of 0.058 +/- 0.005 degrees C center dot yr-1, corresponding to a yearly increase in OHC of 9.43 +/- 0.85 W center dot m-2. The warming of the different water masses will show its feedback on ocean dynamics and air-sea fluxes in the next years, decades, and even centuries as these warming waters spread or re-emerge. This will provide more energy to the atmosphere, resulting in more extreme weather events and will also stress ecosystems and accelerate the extinction of several marine species. This study contributes to a better understanding of climate change in the Mediterranean region, and should act as another wake-up call for policy makers and society.
引用
收藏
页数:14
相关论文
共 50 条
  • [1] Radiative Transfer Modeling With Biogeochemical-Argo Float Data in the Mediterranean Sea
    Terzic, Elena
    Miro, Arnau
    Organelli, Emanuele
    Kowalczuk, Piotr
    D'Ortenzio, Fabrizio
    Lazzari, Paolo
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2021, 126 (10)
  • [2] Horizontal circulation and volume transports in the Weddell Gyre derived : from Argo float data
    Reeve, Krissy Anne
    Boebel, Olaf
    Strass, Volker
    Kanzow, Torsten
    Gerdes, Ruediger
    [J]. PROGRESS IN OCEANOGRAPHY, 2019, 175 : 263 - 283
  • [3] Channel as seen by an Argo Float: Study from Arabian Sea
    Gang, Qiao
    Ismail, Asim
    Zhou, Feng
    Zuo, Liu Song
    [J]. 2013 OCEANS - SAN DIEGO, 2013,
  • [4] Assimilation of Argo float positions in the north western Mediterranean Sea and impact on ocean circulation simulations
    Taillandier, V.
    Griffa, A.
    Poulain, P. -M.
    Beranger, K.
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2006, 33 (11)
  • [5] Hydrography of the Eastern Mediterranean basin derived from argo floats profile data
    Kassis, Dimitris
    Korres, Gerasimos
    [J]. DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2020, 171
  • [6] Bio-optical characterization of subsurface chlorophyll maxima in the Mediterranean Sea from a Biogeochemical-Argo float database
    Barbieux, Marie
    Uitz, Julia
    Gentili, Bernard
    de Fommervault, Orens Pasqueron
    Mignot, Alexandre
    Poteau, Antoine
    Schmechtig, Catherine
    Taillandier, Vincent
    Leymarie, Edouard
    Penkerc'h, Christophe
    D'Ortenzio, Fabrizio
    Claustre, Herve
    Bricaud, Annick
    [J]. BIOGEOSCIENCES, 2019, 16 (06) : 1321 - 1342
  • [7] Seasonal mixed layer temperature and salt balances in the Banda Sea observed by an Argo float
    Ismail, Mochamad Furqon Azis
    Karstensen, Johannes
    Ribbe, Joachim
    Arifin, Taslim
    Chandra, Handy
    Akhwady, Rudhy
    Yulihastin, Erma
    Basit, Abdul
    Budiman, Asep Sandra
    [J]. GEOSCIENCE LETTERS, 2023, 10 (01)
  • [8] Seasonal mixed layer temperature and salt balances in the Banda Sea observed by an Argo float
    Mochamad Furqon Azis Ismail
    Johannes Karstensen
    Joachim Ribbe
    Taslim Arifin
    Handy Chandra
    Rudhy Akhwady
    Erma Yulihastin
    Abdul Basit
    Asep Sandra Budiman
    [J]. Geoscience Letters, 10
  • [9] Towards operational 3D-Var assimilation of chlorophyll Biogeochemical-Argo float data into a biogeochemical model of the Mediterranean Sea
    Cossarini, G.
    Mariotti, L.
    Feudale, L.
    Mignot, A.
    Salon, S.
    Taillandier, V
    Teruzzi, A.
    D'Ortenzio, F.
    [J]. OCEAN MODELLING, 2019, 133 : 112 - 128
  • [10] Deep currents obtained from Argo float trajectories in the Japan/East Sea
    Park, Jong Jin
    Kim, Kuh
    [J]. DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2013, 85 : 169 - 181