Feng Q. He

Sep 9, 2024 | nature.com | Hong Wang |Xu Zhang |Feng Q. He |Lin Liu

AbstractThe last glacial maximum (LGM) is widely acknowledged as the most recent cold period representing maximum global ice conditions. However, substantial warming is observed over Northern Hemisphere. Here, we show that the LGM climate shifted from very cold to fairly warm, followed by less cold conditions in the early Heinrich Stadial 1 (HS1) phases.