Simulated stable water isotopes during the mid-Holocene and pre-industrial periods using AWI-ESM-2.1-wiso

Numerical simulations employing prognostic stable water isotopes can not only facilitate our understanding of hydrological processes and climate change but also allow for a direct comparison between isotope signals obtained from models and various archives. In the current work, we describe the perfo...

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Bibliographic Details
Published in:Geoscientific Model Development 2023-09, Vol.16 (17), p.5153-5178
Main Authors: Shi, Xiaoxu, Cauquoin, Alexandre, Lohmann, Gerrit, Jonkers, Lukas, Wang, Qiang, Yang, Hu, Sun, Yuchen, Werner, Martin
Format: Article
Language:English
Subjects:
African monsoon
Air temperature
Analysis
Archives & records
Boundary conditions
Climate change
Convergence zones
Diurnal variations
General circulation models
Greenhouse gases
Holocene
Hydrologic cycle
Hydrologic processes
Hydrological cycle
Hydrology
Intertropical convergence zone
Isotope composition
Isotopes
Mathematical models
Modelling
Monsoons
Numerical analysis
Numerical simulations
Paleogeography
Phase transitions
Precipitation
Precipitation (Meteorology)
Precipitation variability
Precipitation variations
Seawater
Simulation
Summer
Summer monsoon
Surface temperature
Surface-air temperature relationships
Temperature effects
Tracers
Tracers (Chemistry)
Wind
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Summary:Numerical simulations employing prognostic stable water isotopes can not only facilitate our understanding of hydrological processes and climate change but also allow for a direct comparison between isotope signals obtained from models and various archives. In the current work, we describe the performance and explore the potential of a new version of the Earth system model AWI-ESM (Alfred Wegener Institute Earth System Model), labeled AWI-ESM-2.1-wiso, in which we incorporated three isotope tracers into all relevant components of the water cycle. We present here the results of pre-industrial (PI) and mid-Holocene (MH) simulations. The model reproduces the observed PI isotope compositions in both precipitation and seawater well and captures their major differences from the MH conditions. The simulated relationship between the isotope composition in precipitation (δ18Op) and surface air temperature is very similar between the PI and MH conditions, and it is largely consistent with modern observations despite some regional model biases. The ratio of the MH–PI difference in δ18Op to the MH–PI difference in surface air temperature is comparable to proxy records over Greenland and Antarctica only when summertime air temperature is considered. An amount effect is evident over the North African monsoon domain, where a negative correlation between δ18Op and the amount of precipitation is simulated. As an example of model applications, we studied the onset and withdrawal date of the MH West African summer monsoon (WASM) using daily variables. We find that defining the WASM onset based on precipitation alone may yield erroneous results due to the substantial daily variations in precipitation, which may obscure the distinction between pre-monsoon and monsoon seasons. Combining precipitation and isotope indicators, we suggest in this work a novel method for identifying the commencement of the WASM. Moreover, we do not find an obvious difference between the MH and PI periods in terms of the mean onset of the WASM. However, an advancement in the WASM withdrawal is found in the MH compared to the PI period due to an earlier decline in insolation over the northern location of Intertropical Convergence Zone (ITCZ).
ISSN:1991-9603
1991-959X
1991-962X
1991-9603
1991-962X
DOI:10.5194/gmd-16-5153-2023