• Mashup Score: 1

    The weathering alkalinity flux from mid-latitudes to the ocean will be strongly altered by climate warming by 2100. Under different emissions scenarios either a strengthening or a weakening of the flux and thus of the oceanic CO2 buffer is predicted.

    Tweet Tweets with this article
    • The #weathering #erosion #alkalinity flux from mid-latitudes to the ocean will be strongly altered by #climatewarming, different emissions scenarios predict either a strengthening or a weakening of the flux and oceanic CO2 buffer @HereonHelmholtz @AWI_de https://t.co/pi2m1by5PG https://t.co/HbCVJvLRPv