The longevity of naturally occurring carbon sinks, like those in Earth’s forests, is a key part of all modeled and projected pathways to net-zero. Without the considerable carbon absorption capacity of our lands (and oceans), we’d currently have much more CO2 in the atmosphere and an accelerated timeline of warming.
But the complexities of the interactions between the land and atmosphere, especially in a rapidly changing climate, are challenging to model, leading to uncertainty around the magnitude and persistence of this critical carbon sink. I dug into this complexity with my energy colleagues in the context of their recent analysis of pathways for how the US can meet its goals to cut heat-trapping emissions 50%-52% below 2005 levels by 2030, and achieve net zero emissions no later than 2050.
That analysis assumed the U.S. land sink stays fixed at current…
Read the full article originally published at blog.ucsusa.org.