The isotopic signature of monsoon conditions, cloud modes, and rainfall type

Costijn Zwart, Niels C. Munksgaard, Alain Protat, Naoyuki Kurita, Dionisia Lambrinidis, Michael I. Bird

    Research output: Contribution to journalArticleResearchpeer-review

    Abstract

    This work provides a comprehensive physically based framework for the interpretation of the north Australian rainfall stable isotope record (δ18O and δ2H). Until now, interpretations mainly relied on statistical relationships between rainfall amount and isotopic values on monthly timescales. Here, we use multiseason daily rainfall stable isotope and high resolution (10 min) ground-based C-band polarimetric radar data and show that the five weather types (monsoon regimes) that constitute the Australian wet season each have a characteristic isotope ratio. The data suggest that this is not only due to changes in regional rainfall amount during these regimes but, more importantly, is due to different rain and cloud types that are associated with the large scale circulation regimes. Negative (positive) isotope anomalies occurred when stratiform rainfall fractions were large (small) and the horizontal extent of raining areas were largest (smallest). Intense, yet isolated, convective conditions were associated with enriched isotope values whereas more depleted isotope values were observed when convection was widespread but less intense. This means that isotopic proxy records may record the frequency of which these typical wet season regimes occur. Positive anomalies in paleoclimatic records are most likely associated with periods where continental convection dominates and convection is sea-breeze forced. Negative anomalies may be interpreted as periods when the monsoon trough is active, convection is of the oceanic type, less electric, and stratiform areas are wide spread. This connection between variability of rainfall isotope anomalies and the intrinsic properties of convection and its large-scale environment has important implications for all fields of research that use rainfall stable isotopes.

    Original languageEnglish
    Pages (from-to)2296-2303
    Number of pages8
    JournalHydrological Processes
    Volume32
    Issue number15
    Early online date14 May 2018
    DOIs
    Publication statusPublished - 15 Jul 2018

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    monsoon
    rainfall
    convection
    isotope
    anomaly
    stable isotope
    wet season
    sea breeze
    trough
    radar
    timescale
    weather

    Cite this

    Zwart, C., Munksgaard, N. C., Protat, A., Kurita, N., Lambrinidis, D., & Bird, M. I. (2018). The isotopic signature of monsoon conditions, cloud modes, and rainfall type. Hydrological Processes, 32(15), 2296-2303. https://doi.org/10.1002/hyp.13140
    Zwart, Costijn ; Munksgaard, Niels C. ; Protat, Alain ; Kurita, Naoyuki ; Lambrinidis, Dionisia ; Bird, Michael I. / The isotopic signature of monsoon conditions, cloud modes, and rainfall type. In: Hydrological Processes. 2018 ; Vol. 32, No. 15. pp. 2296-2303.
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    Zwart, C, Munksgaard, NC, Protat, A, Kurita, N, Lambrinidis, D & Bird, MI 2018, 'The isotopic signature of monsoon conditions, cloud modes, and rainfall type', Hydrological Processes, vol. 32, no. 15, pp. 2296-2303. https://doi.org/10.1002/hyp.13140

    The isotopic signature of monsoon conditions, cloud modes, and rainfall type. / Zwart, Costijn; Munksgaard, Niels C.; Protat, Alain; Kurita, Naoyuki; Lambrinidis, Dionisia; Bird, Michael I.

    In: Hydrological Processes, Vol. 32, No. 15, 15.07.2018, p. 2296-2303.

    Research output: Contribution to journalArticleResearchpeer-review

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    Zwart C, Munksgaard NC, Protat A, Kurita N, Lambrinidis D, Bird MI. The isotopic signature of monsoon conditions, cloud modes, and rainfall type. Hydrological Processes. 2018 Jul 15;32(15):2296-2303. https://doi.org/10.1002/hyp.13140