Interpreting H2O isotope variations in high‐altitude ice cores using a cyclone model

[1] Vertical profiles of isotope (δ18O or δD) values versus altitude (z) from sea level to high altitude provide a link to cyclones, which impact most ice core sites. Cyclonic structure variations cause anomalous variations in ice core δ time series which may obscure the basic temperature signal. Only one site (Mount Logan, Yukon) provides a complete δ versus z profile generated solely from data. At other sites, such a profile has to be constructed by supplementing field data. This requires using the so-called isotopic or δ thermometer which relates δ to a reference temperature (T). The construction of gapped sections of δ versus z curves requires assuming a typical atmospheric lapse rate (dT/dz), where T is air temperature, and using the slope (dδ/dT) of a site-derived δ thermometer to calculate dδ/dz. Using a three-layer model of a cyclone, examples are given to show geometrically how changes in the thickness of the middle, mixed layer leads to the appearance of anomalous δ values in time series (producing decalibration of the δ thermometer there). The results indicate that restrictions apply to the use of the δ thermometer in ice core paleothermometry, according to site altitude, regional meteorology, and climate state.