Library

Welcome to Climanosco’s library, an ever-growing collection on all things climate science.

Topics

 

Sea level under climate change: Understanding the links between the past and the future

Keven Roy, Nicole S. Khan, Timothy A. Shaw, Robert E. Kopp and Benjamin P. Horton

Rising global sea level, a consequence of climate change, results from an increase in the world ocean’s water volume and mass. Recent climate warming is responsible for producing the highest rate of global average sea-level rise of the past few millennia, and this rate will accelerate through the 21st century and beyond, exposing low-lying islands and coastal regions to significant …

Continue reading “Sea level under climate change: Understanding the links between the past and the future”

What do historical temperature records tell us about natural variability in global temperature?

Patrick T Brown

Global average surface air temperature can change when it is either ‘forced’ to change by factors such as increasing greenhouse gasses, or it can change on its own through ‘unforced’ natural cycles like El-Niño/La-Niña. In this paper we estimated the magnitude of unforced temperature variability using historical datasets rather than the more commonly used computer climate models. We used data …

Continue reading “What do historical temperature records tell us about natural variability in global temperature?”

The impact of climate change on Australian Aboriginal hunter-gatherers and their response over the last 35,000 years.

Alan N Williams

In a recent article, I (and my colleagues) present models of population change for key regions across Australia over the last 35,000 years. We use these models to test an archaeological method (the use of numbers of radiocarbon dates as an indicator of human behaviour), explore the relationship of Aboriginal people and climate change, and to provide a status update …

Continue reading “The impact of climate change on Australian Aboriginal hunter-gatherers and their response over the last 35,000 years.”

Global warming might be on hold, but it’s not cancelled

Iselin Medhaug

Instrumental measurements of surface temperatures are available back to around 1850. Based on these, we can estimate the annual mean global temperature. Global temperatures are clearly rising, mainly because of increasing amounts of greenhouse gases, like for example CO2 and methane, from use of coal, oil and gas and deforestation. Since 1998, a paradox seems to have appeared, where the …

Continue reading “Global warming might be on hold, but it’s not cancelled”