{"id":3752,"date":"2023-05-31T19:59:04","date_gmt":"2023-05-31T17:59:04","guid":{"rendered":"https:\/\/www.co2news.sk\/?p=3752"},"modified":"2023-05-31T19:59:04","modified_gmt":"2023-05-31T17:59:04","slug":"increasingly-negative-relationship-between-tropical-water-and-growth-rate","status":"publish","type":"post","link":"https:\/\/www.co2news.sk\/en\/2023\/05\/31\/increasingly-negative-relationship-between-tropical-water-and-growth-rate\/","title":{"rendered":"Increasingly negative relationship between tropical water and CO growth rate"},"content":{"rendered":"<p><span>Terrestrial ecosystems have absorbed approximately 32 % of total anthropogenic CO emissions over the past six decades\u00a0<\/span><sub><span>2\u00a0<\/span><\/sub><sup><a id=\"ref-link-section-d16885522e518\" title=\"Friedlingstein, P. et al. Global Carbon Budget 2020. Earth Syst. Sci. Data 12, 3269\u20133340 (2020).\" href=\"https:\/\/www.nature.com\/articles\/s41586-023-06056-x#ref-CR1\" data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Link 1\" target=\"_blank\" rel=\"noopener\"><span>1<\/span><\/a><\/sup><span>\u00a0. However, large uncertainties in terrestrial carbon\u2013climate feedbacks make it difficult to predict how terrestrial carbon sequestration will respond to future climate change\u00a0<\/span><sup><a id=\"ref-link-section-d16885522e522\" title=\"Friedlingstein, P. et al. Analysis of climate-carbon feedbacks: results from the model intercomparison (CMIP)-M-4. J. Clim. 19, 3337-3353 (2006).\" href=\"https:\/\/www.nature.com\/articles\/s41586-023-06056-x#ref-CR2\" data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Link 2\" target=\"_blank\" rel=\"noopener\"><span>2<\/span><\/a><\/sup><span>\u00a0. Interannual changes in the growth rate of atmospheric CO\u00a0<\/span><sub><span>2<\/span><\/sub><span>\u00a0(CGR) are dominated by land-atmosphere carbon fluxes in the tropics, providing an opportunity to investigate carbon-climate interactions on land\u00a0<\/span><sup><a id=\"ref-link-section-d16885522e528\" title=\"Bousquet, P. et al. Regional changes in land and ocean carbon dioxide fluxes since 1980. Science 290, 1342\u20131346 (2000).\" href=\"https:\/\/www.nature.com\/articles\/s41586-023-06056-x#ref-CR3\" data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" target=\"_blank\" rel=\"noopener\"><span>3<\/span><\/a><span>\u00a0,\u00a0<\/span><a id=\"ref-link-section-d16885522e528_1\" title=\"Piao, SL et al. Interannual variations of the Earth&#039;s carbon cycle: Issues and perspectives. Glob. Change Biol. 26, 300\u2013318 (2020).\" href=\"https:\/\/www.nature.com\/articles\/s41586-023-06056-x#ref-CR4\" data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" target=\"_blank\" rel=\"noopener\"><span>4<\/span><\/a><span>\u00a0,\u00a0<\/span><a id=\"ref-link-section-d16885522e528_2\" title=\"Cox, PM et al. Sensitivity of tropical carbon to climate change constrained by carbon dioxide variability. Nature 494, 341\u2013344 (2013).\" href=\"https:\/\/www.nature.com\/articles\/s41586-023-06056-x#ref-CR5\" data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" target=\"_blank\" rel=\"noopener\"><span>5<\/span><\/a><span>\u00a0,\u00a0<\/span><a id=\"ref-link-section-d16885522e531\" title=\"Canadell, JG et al. in Climate Change 2021: The Physical Science Basis (eds Masson-Delmotte, V. et al.) 673\u2013816 (Cambridge Univ. Press, 2021).\" href=\"https:\/\/www.nature.com\/articles\/s41586-023-06056-x#ref-CR6\" data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Link 6\" target=\"_blank\" rel=\"noopener\"><span>6<\/span><\/a><\/sup><span>\u00a0. CGR changes are believed to be largely controlled by temperature\u00a0<\/span><sup><a id=\"ref-link-section-d16885522e536\" title=\"Wang, WL et al. Changes in the growth rate of atmospheric CO2 associated with tropical temperature. Proc. Natl Acad. Sci. USA 110, 13061\u201313066 (2013).\" href=\"https:\/\/www.nature.com\/articles\/s41586-023-06056-x#ref-CR7\" data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" target=\"_blank\" rel=\"noopener\"><span>7<\/span><\/a><span>\u00a0,\u00a0<\/span><a id=\"ref-link-section-d16885522e536_1\" title=\"Anderegg, WRL et al. Tropical nocturnal warming as a dominant driver of variability in the terrestrial carbon sink. Proc. Natl Acad. Sci. USA 112, 15591\u201315596 (2015).\" href=\"https:\/\/www.nature.com\/articles\/s41586-023-06056-x#ref-CR8\" data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" target=\"_blank\" rel=\"noopener\"><span>8<\/span><\/a><span>\u00a0,\u00a0<\/span><a id=\"ref-link-section-d16885522e536_2\" title=\"Jung, M. et al. The compensatory effects of water link the annual global changes in the decrease of CO2 to the earth with temperature. Nature 541, 516\u2013520 (2017).\" href=\"https:\/\/www.nature.com\/articles\/s41586-023-06056-x#ref-CR9\" data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" target=\"_blank\" rel=\"noopener\"><span>9<\/span><\/a><span>,\u00a0<\/span><a id=\"ref-link-section-d16885522e539\" title=\"Braswell, BH, Schimel, DS, Linder, E. &amp; Moore, B. Response of global terrestrial ecosystems to interannual temperature variability. Science 278, 870-872 (1997).\" href=\"https:\/\/www.nature.com\/articles\/s41586-023-06056-x#ref-CR10\" data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 10\" target=\"_blank\" rel=\"noopener\"><span>10<\/span><\/a><\/sup><span>\u00a0, but there is also evidence of a close relationship between water availability and CGR\u00a0<\/span><sup><a id=\"ref-link-section-d16885522e543\" title=\"Humphrey, V. et al. Sensitivity of atmospheric CO2 growth rate to observed changes in terrestrial water storage. Nature 560, 628-631 (2018).\" href=\"https:\/\/www.nature.com\/articles\/s41586-023-06056-x#ref-CR11\" data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 11\" target=\"_blank\" rel=\"noopener\"><span>11<\/span><\/a><\/sup><span>\u00a0. Here we use records of global atmospheric CO\u00a0<\/span><sub><span>2<\/span><\/sub><span>\u00a0, terrestrial water storage, and precipitation data to investigate changes in the interannual relationship between tropical landscape climatic conditions and CGR in a changing climate. We find that the interannual relationship between tropical water availability and CGR has become increasingly negative in 1989\u20132018 compared to 1960\u20131989. This could be related to spatiotemporal changes in tropical water availability anomalies caused by shifts in the El Ni\u00f1o\/Southern Oscillation teleconnection, including decreasing spatial compensatory effects of water\u00a0<\/span><sup><a id=\"ref-link-section-d16885522e549\" title=\"Jung, M. et al. The compensatory effects of water link the annual global changes in the decrease of CO2 to the earth with temperature. Nature 541, 516\u2013520 (2017).\" href=\"https:\/\/www.nature.com\/articles\/s41586-023-06056-x#ref-CR9\" data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Link 9\" target=\"_blank\" rel=\"noopener\"><span>9<\/span><\/a><\/sup><span>.\u00a0<\/span><\/p>\n<p><em>(Laibao Liu, Philippe Ciais, Sonia I. Seneviratne)<\/em><\/p>","protected":false},"excerpt":{"rendered":"<p>Terrestrial ecosystems have absorbed approximately 32 % of total anthropogenic CO 2 emissions over the past six decades 1 . However, large uncertainties in the feedbacks between terrestrial carbon and climate make it difficult to predict how terrestrial carbon sequestration will respond to future climate change 2 . Interannual changes in the rate of growth of atmospheric CO 2 (CGR) are dominated by land-atmosphere carbon fluxes in the tropics, providing an opportunity [\u2026]<\/p>","protected":false},"author":7,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[4],"tags":[],"class_list":["post-3752","post","type-post","status-publish","format-standard","hentry","category-klimaticka-zmena"],"acf":[],"_links":{"self":[{"href":"https:\/\/www.co2news.sk\/en\/wp-json\/wp\/v2\/posts\/3752","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.co2news.sk\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.co2news.sk\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.co2news.sk\/en\/wp-json\/wp\/v2\/users\/7"}],"replies":[{"embeddable":true,"href":"https:\/\/www.co2news.sk\/en\/wp-json\/wp\/v2\/comments?post=3752"}],"version-history":[{"count":0,"href":"https:\/\/www.co2news.sk\/en\/wp-json\/wp\/v2\/posts\/3752\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.co2news.sk\/en\/wp-json\/wp\/v2\/media?parent=3752"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.co2news.sk\/en\/wp-json\/wp\/v2\/categories?post=3752"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.co2news.sk\/en\/wp-json\/wp\/v2\/tags?post=3752"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}