On borrowed time: How long to a Miocene-like tropical ~+4°C world?

1. increased evaporation with warming, water vapor being a greenhouse gas;
2. melting ice decreasing the albedo effect of Earth, exposing dark rock surfaces, reducing the albedo of the polar terrains and sea ice in surrounding oceans, enhancing infrared absorption and heating;
3. burnt and desiccated vegetation decreasing the albedo;
4. decreased absorption and solubility of CO₂ in warming oceans;
5. release of CO₂ and methane from drying vegetation, from melting permafrost and from bogs.

A critical parameter, rarely mentioned in the media, is the inexorable accelerating rise in atmospheric greenhouse gases. With CO₂ reaching 414.6 parts per million, CH₄ (methane) is reaching 1891.3 parts per billion and total greenhouse gas concentration of 500 parts per million, a level unknown since the Miocene about 5.3-23 million years ago.

With a Miocene CO₂ level in the range of ~400-500 parts per million and mean temperatures up to 18.4°C, the atmosphere is tracking toward super-tropical temperatures, which would render large regions uninhabitable.

Anthropocene temperature rise rates are at least an order of magnitude higher than the mean temperature rise since the Last Glacial Maximum:

• Given the current mean global land and ocean temperature of 14°C, i.e. 6.2°C warmer than the mean ~7.8°C temperature of the Last Glacial Maximum (LGM) (~19,000–23.000 years-ago), the mean warming of (~0.00026°C/year rate; 6°C/23.000 years) is an order of magnitude slower than during the Anthropocene.
• Late Holocene/Anthropocene: 1.04°C/250 years ~0.004°C/year). This relegates the current global warming to an unprecedented category during the last ~3 million years and longer.

Namely, at ~+4 degrees Celsius of warming toward later the 21st century the Earth’s mean surface land/ocean temperature would be warmer than tropical Miocene temperatures. A lag effect between the rise of greenhouse gases and temperature would delay but not prevent the worst effects of global warming.

But even before such high mean temperatures is reached, the weakened jet stream climate zone boundary, allowing penetration of cold and warm fronts, allowing clashes between air and water masses of contrasting temperatures, would lead to storminess, disrupting human agriculture and habitats, as is already happening in northern Europe and within the Arctic circle. 

How long would it take for global temperatures to rise to about ~4°C and higher would depend on:

1. The acceleration in rising concentration of greenhouse gases and the lag in consequent rising temperatures;
2. The extent to which ice melt flow from Greenland and Antarctica may slow down further warming in certain regions, such as the north Atlantic and the Southern Ocean;
3. Further anthropogenic emissions and/or draw-down of atmospheric CO₂.