Author Archives: Rolf Schuttenhelm

Tropical forest CO2 fertilisation: self-mitigation of emissions possibly around 15 percent

In which case increased tropical forest density would sort of average out emissions of tropical deforestation. [Is it just us or do you share the feeling something is uncomfortably unsustainable about that comparison?] A couple of days ago we reported … Continue reading →

NASA climate model study: Arctic melting linear with temperature

Here’s another climate model study that challenges the Arctic tipping point idea. Arctic melting is still sensitive to temperature rise though and any further increase in atmospheric CO2 will keep translating to further ice loss. According to the new NASA … Continue reading →

Climate model shows possibility of multiple years of Arctic sea ice growth – or faster decline

Computer simulations of the US National Center for Atmospheric Research indicate that the natural Arctic climate variability, like seasonal and annual variations in pressure systems, wind patterns and precipitation or cloud cover, could be larger than previously thought.

Permian-Triassic mass extinction: 11,000 Gt CO2 worth of climate change led to microbial plagues that killed the world’s forests

New research shows an example of a missing link between climatic disruptions and biodiversity decline: killer microbes.

Fossil driftwood tells Danish scientists the Arctic sea ice variations during Holocene are larger than we thought

During the Holocene Climatic Optimum of 8,000 to 5,000 years ago, the Arctic sea ice was less than 50% [so <2.6 mln sq km] of the lowest extent on satellite record, the 2007 melting record, researchers of Copenhagen University stated … Continue reading →

Crop geoengineering #3: doubling root depth would store 230 Gt carbon in agricultural soils – minus 118 ppm CO2

Breeding crops with deeper (and larger) root systems could help to lower atmospheric CO2 levels, while also making the crops better drought-resistant, Douglas Kell, a Professor of Bioanalytical Science at the University of Manchester says.

Lull in upper ocean warming explained through ENSO – warming trend continues

Shortly after an El Niño event there is elevated heat exchange from the upper ocean layers to the cosmos over the tropical Pacific Ocean. In the North Atlantic Ocean, variations in the ocean circulation affect the heat exchange to the … Continue reading →