Stable Water Isotope Signals and Their Relation to Stratiform and Convective Precipitation in the Tropical Andes

Landshuter N, Aemisegger F, Mölg T (2024)

Publication Type: Journal article

Publication year: 2024

Journal

Journal of Geophysical Research: Atmospheres American Geophysical Union (AGU)

Book Volume: 129

Article Number: e2023JD040630

Journal Issue: 14

DOI: 10.1029/2023JD040630

Abstract

Stratiform and convective precipitation are known to be associated with distinct isotopic fingerprints in the tropics. Such rain type specific isotope signals are of key importance for climate reconstructions derived from climate proxies (e.g., stable isotopes in tree rings). Recently, the relation between rain type and isotope signal in present-day climate has been intensively discussed. While some studies point out the importance of deep convection, other studies emphasize the role of stratiform precipitation for strongly depleted isotope signals in precipitation. Uncertainties arise from observational studies due to data scarcity while modeling approaches with global climate models cannot explicitly resolve convective processes and rely on parameterizations. High-resolution climate models are particularly important for studies over complex topography and for the simulation of convective cloud formation and organization. Therefore, we applied the isotope-enabled version of the high-resolution climate model from the Consortium for Small-Scale Modeling (COSMOiso) over the Andes of tropical south Ecuador, South America, to investigate the influence of stratiform and convective rain on the stable oxygen isotope signal of precipitation (δ18OP). Our results highlight the importance of deep convection for depleting the isotopic signal of precipitation and increasing its deuterium excess. Due to the opposing effect of shallow and deep convection on the δ18OP signal, the use of a stratiform fraction might be misleading. We therefore propose to use a shallow and deep convective fraction to analyze the effect of rain types on δ18OP.

Authors with CRIS profile

Nadja Landshuter Institut für Geographie Thomas Mölg Professur für Geographie

Involved external institutions

Eidgenössische Technische Hochschule Zürich (ETHZ) / Swiss Federal Institute of Technology in Zurich CH Switzerland (CH)

How to cite

APA:

Landshuter, N., Aemisegger, F., & Mölg, T. (2024). Stable Water Isotope Signals and Their Relation to Stratiform and Convective Precipitation in the Tropical Andes. Journal of Geophysical Research: Atmospheres, 129(14). https://doi.org/10.1029/2023JD040630

MLA:

Landshuter, Nadja, Franziska Aemisegger, and Thomas Mölg. "Stable Water Isotope Signals and Their Relation to Stratiform and Convective Precipitation in the Tropical Andes." Journal of Geophysical Research: Atmospheres 129.14 (2024).

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