Higher temperatures caused by anthropogenic climate change turned an ordinary drought into an exceptional one that parched the American West from 2020–22. A study by UCLA and NOAA scientists has found that evaporation accounted for 61% of the drought’s severity, while reduced precipitation accounted for 39%. The research found that since 2000, evaporative demand has played a bigger role than reduced precipitation in droughts, which may become more severe as the climate warms.

While atmospheric carbon dioxide (CO2) levels are higher than ever before, an estimated 2.5 billion additional people are expected to integrate into urban areas worldwide by 2050, making reduced urban CO2 emissions a priority. A group of scientists investigated the effects of urban form, specifically at the building and street level, on urban carbon emissions using detailed assessment methods in three different U.S. cities. The results demonstrate that the relationship between urban form and CO2 emissions is complex and dynamic. Patterns could be different depending on the context and factors such as climatic conditions and size and function of the city. This means that one-size-fits-all approaches cannot be applied to determine optimized urban forms.

At the end of the last global ice age, the deep-frozen Earth reached a built-in limit of climate change and thawed into a slushy planet. Results from a Virginia Tech-led study provide the first direct geochemical evidence of the slushy planet — otherwise known as the “plumeworld ocean” era — when sky-high carbon dioxide levels forced the frozen Earth into a massive, rapid melting period.