Abstract. We quantify retreat rates for three alpine glaciers in the Sawatch Range of
the southern Rocky Mountains following the Last Glacial Maximum using
10Be ages from ice-sculpted, valley-floor bedrock transects and
statistical analysis via the BACON program in R. Glacier retreat in the
Sawatch Range from at (100 %) or near (∼83 %) Last
Glacial Maximum extents initiated between 16.0 and 15.6 ka and was complete
by 14.2–13.7 ka at rates ranging between 35.6 and 6.8 m a−1.
Deglaciation in the Sawatch Range commenced ∼2–3 kyr later
than the onset of rising global CO2 and prior to rising temperatures
observed in the North Atlantic region at the Heinrich Stadial 1–Bølling
transition. However, deglaciation in the Sawatch Range approximately aligns
with the timing of Great Basin pluvial lake lowering. Recent data–modeling
comparison efforts highlight the influence of the large North American ice
sheets on climate in the western United States, and we hypothesize that
recession of the North American ice sheets may have influenced the timing
and rate of deglaciation in the Sawatch Range. While we cannot definitively
argue for exclusively North Atlantic forcing or North American ice sheet
forcing, our data demonstrate the importance of regional forcing mechanisms
for past climate records.
Abstract. We quantify retreat rates for three alpine glaciers in the Sawatch Range of the southern Rocky Mountains following the Last Glacial Maximum using 10Be ages from ice-sculpted, valley-floor bedrock transects and statistical analysis via the BACON program in R. Glacier retreat in the Sawatch Range from at (100 %) or near (~ 83 %) Last Glacial Maximum extents initiated between 16.3 and 15.6 ka and was complete by 14.2–13.7 ka at rates ranging between 9.9 and 19.8 m a−1. Deglaciation in the Sawatch Range commenced ~ 2–3 kyr later than the onset of rising global CO2, but approximately in-step with rising temperatures observed in the North Atlantic region at the Heinrich Stadial 1/Bølling transition. Our results highlight a possible teleconnection between the North Atlantic sector and the southern Rocky Mountains. However, deglaciation in the Sawatch Range also approximately aligns with the timing of Great Basin pluvial lake lowering. Recent data-modeling comparison efforts highlight the influence of the large North American ice sheets on climate in the western United States, and we hypothesize that recession of the North American ice sheets may have influenced the timing and rate of deglaciation in the Sawatch Range. While we cannot definitively argue for exclusively North Atlantic forcing or North American ice sheet forcing, our data demonstrate the importance of regional forcing mechanisms on past climate records.
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