In a seminal study published in Nature Geoscience, researchers, led by Victoria Todd from the University of Texas at Austin, propose that the drought is impacted by persistent warm temperature patterns in the Pacific Ocean, which could lead to moisture deficits lasting well into the latter half of the century and potentially beyond. Todd argues that the driving force behind this sustained dry spell is a “stuck” pattern of ocean temperatures, exacerbated by human-induced climate change.
To uncover the origins of this current dry period, researchers analyzed sediment from two lakes—Stewart Bog in New Mexico and Hunters Lake in Colorado. Through examining the chemical signatures embedded in ancient plant material, they reconstructed climate conditions over the past 14,000 years. Their findings reveal that similar prolonged drought conditions occurred in the past under warm climates, caused by shifts in solar radiation and ocean temperatures, which resulted in changes to jet streams that deflected storms away from the Southwest.
Additional simulations demonstrated that a significant warm water mass in the Pacific—referred to as the negative phase of the Pacific Decadal Oscillation—could remain fixed due to the current trajectory of global warming. This “blob” is likely to exacerbate existing drought conditions, significantly underestimating future drought risks in the Southwest.
Climate experts emphasize that rising temperatures are causing adverse effects beyond typical historical patterns, such as reducing snow accumulation during precipitation events and increasing evaporation rates. Observations during the 2023-2024 El Niño, which usually brings wetter conditions to the region, did not yield expected weather patterns, indicating a potential shift in climate responses due to anthropogenic influences.
As the implications of this research unfold, it highlights the urgency for understanding and addressing how human activity may be altering established climate systems, challenging the standard perceptions of drought cycles in the American Southwest.
To uncover the origins of this current dry period, researchers analyzed sediment from two lakes—Stewart Bog in New Mexico and Hunters Lake in Colorado. Through examining the chemical signatures embedded in ancient plant material, they reconstructed climate conditions over the past 14,000 years. Their findings reveal that similar prolonged drought conditions occurred in the past under warm climates, caused by shifts in solar radiation and ocean temperatures, which resulted in changes to jet streams that deflected storms away from the Southwest.
Additional simulations demonstrated that a significant warm water mass in the Pacific—referred to as the negative phase of the Pacific Decadal Oscillation—could remain fixed due to the current trajectory of global warming. This “blob” is likely to exacerbate existing drought conditions, significantly underestimating future drought risks in the Southwest.
Climate experts emphasize that rising temperatures are causing adverse effects beyond typical historical patterns, such as reducing snow accumulation during precipitation events and increasing evaporation rates. Observations during the 2023-2024 El Niño, which usually brings wetter conditions to the region, did not yield expected weather patterns, indicating a potential shift in climate responses due to anthropogenic influences.
As the implications of this research unfold, it highlights the urgency for understanding and addressing how human activity may be altering established climate systems, challenging the standard perceptions of drought cycles in the American Southwest.
