Details

Autor(en) / Beteiligte

• Zhu, Jiang
• Liu, Zhengyu
• Brady, Esther C.
• Otto‐Bliesner, Bette L.
• Marcott, Shaun A.
• Zhang, Jiaxu
• Wang, Xianfeng
• Nusbaumer, Jesse
• Wong, Tony E.
• Jahn, Alexandra
• Noone, David

Titel

Investigating the Direct Meltwater Effect in Terrestrial Oxygen‐Isotope Paleoclimate Records Using an Isotope‐Enabled Earth System Model

Ist Teil von

• Geophysical research letters, 2017-12, Vol.44 (24), p.12,501-12,510

Ort / Verlag

Washington: John Wiley & Sons, Inc

Erscheinungsjahr

2017

Quelle

Wiley Online Library

Beschreibungen/Notizen

• Variations in terrestrial oxygen‐isotope reconstructions from ice cores and speleothems have been primarily attributed to climatic changes of surface air temperature, precipitation amount, or atmospheric circulation. Here we demonstrate with the fully coupled isotope‐enabled Community Earth System Model an additional process contributing to the oxygen‐isotope variations during glacial meltwater events. This process, termed “the direct meltwater effect,” involves propagating large amounts of isotopically depleted meltwater throughout the hydrological cycle and is independent of climatic changes. We find that the direct meltwater effect can make up 15–35% of the δ18O signals in precipitation over Greenland and eastern Brazil for large freshwater forcings (0.25–0.50 sverdrup (106 m3/s)). Model simulations further demonstrate that the direct meltwater effect increases with the magnitude and duration of the freshwater forcing and is sensitive to both the location and shape of the meltwater. These new modeling results have important implications for past climate interpretations of δ18O. Key Points A portion of the δ18O signal in land‐based paleoclimate proxies can be attributed to the direct meltwater effect instead of climatic changes The direct meltwater effect can make up 15‐35% of the δ18O signals in precipitation in Greenland and eastern Brazil for large meltwater events The direct meltwater effect increases with the magnitude and duration of the freshwater forcing and is sensitive to location and shape dependent