Posters note: relevant to the interplay between SRM and CDR, specifically
as regards tolerable levels of drying - and thus which technologies are
most appropriate

https://www.nature.com/articles/s41586-018-0424-4

Letter | Published: 29 August 2018

Sensitivity of atmospheric CO2 growth rate to observed changes in
terrestrial water storage
Vincent Humphrey, Jakob Zscheischler, […]Sonia I. Seneviratne
Naturevolume 560, pages628–631 (2018) | Download Citation

Abstract
Land ecosystems absorb on average 30 per cent of anthropogenic carbon
dioxide (CO2) emissions, thereby slowing the increase of CO2 concentration
in the atmosphere1. Year-to-year variations in the atmospheric CO2 growth
rate are mostly due to fluctuating carbon uptake by land ecosystems1. The
sensitivity of these fluctuations to changes in tropical temperature has
been well documented2,3,4,5,6, but identifying the role of global water
availability has proved to be elusive. So far, the only usable proxies for
water availability have been time-lagged precipitation anomalies and
drought indices3,4,5, owing to a lack of direct observations. Here, we use
recent observations of terrestrial water storage changes derived from
satellite gravimetry7 to investigate terrestrial water effects on carbon
cycle variability at global to regional scales. We show that the CO2 growth
rate is strongly sensitive to observed changes in terrestrial water
storage, drier years being associated with faster atmospheric CO2 growth.
We demonstrate that this global relationship is independent of known
temperature effects and is underestimated in current carbon cycle models.
Our results indicate that interannual fluctuations in terrestrial water
storage strongly affect the terrestrial carbon sink and highlight the
importance of the interactions between the water and carbon cycles.

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