Jul 9, 2020 · Quantifying CO2 levels during the mid-Piacenzian Warm Period (mPWP) provides a means, therefore, to deepen our understanding of Earth System behaviour in a warm climate state.

The Mid-Piacenzian Warm Period (mPWP) (prior to 2009 known as the Middle Pliocene Warm Period ), or the Pliocene Thermal Maximum, was an interval of warm climate during the Pliocene epoch that lasted from 3.3 to 3.0 million years ago (Ma).

Feb 16, 2016 · The mid-Pliocene Warm Period (mPWP) offers an opportunity to understand a warmer-than-present world and assess the predictive ability of numerical climate models.

Jun 22, 2024 · The mid-Piacenzian Warm Period (MPWP, ~ 3.264–3.025 Ma) is the most recent example of a persistently warmer climate in equilibrium wit

Feb 16, 2016 · The mid-Pliocene Warm Period (mPWP) offers an opportunity to understand a warmer-than-present world and assess the predictive ability of numerical climate models. Environmental reconstruction and climate modelling are crucial for understanding the mPWP, and the synergy of these two, often disparate, …

May 15, 2024 · Documenting the seasonal temperature cycle constitutes an essential step toward mitigating risks associated with extreme weather events in a future warmer world. The mid-Piacenzian Warm Period (mPWP), 3.3 to 3.0 million years ago, featured global temperatures approximately 3°C above preindustrial levels.

Feb 10, 2024 · Based on 12 climate model outputs from Pliocene Model Intercomparison Project Phase 2 (PlioMIP2), we investigate tropical atmospheric circulation (TAC) changes under the warm MPWP and associated underlying mechanisms by diagnosing both atmospheric static stability and diabatic processes.

Aug 15, 2011 · The MPWP (also referred to as the PRISM interval) is an interval of warm and stable climate between 3.264 Ma and 3.025 Ma. This interval occurs prior to the first strong oxygen isotope excursions, which represent a change toward modern conditions of intensified glacial–interglacial variation (Sancetta and Silvestri, 1986, Raymo et al., 1989 ...

Mar 1, 2020 · The mid-Pliocene Warm Period (mPWP; also referred to as the mid-Piacenzian Warm Period) is widely recognised as a geological example of a warmer world that, in fundamental ways, parallels climate model simulations of this century (Haywood et al., 2013a).

在上新世中期暖期（MPWP;3.3~3.0 MaBP),全球平均地表温度（GMST）比1850—1990年高2.5~4.0℃,GMSL比当前高5~25 m。 冰盖模式结果表明格陵兰和西南极冰盖几乎都已消融,东南极物质也有部分损失。