Exploring New Zealand Climate Change in Groundwater

Alan Seltzer, a senior at Columbia University, traveled to New Zealand this past summer to work on field experiments aimed at reconstructing temperatures in the region over the last 20,000 years. His adviser, geochemist Martin Stute, is working closely with colleagues at Lamont-Doherty to understand how the southern hemisphere came out of the last ice age.

By
Guest Blogger
October 03, 2013

By Alan Seltzer

Noble gases, the elements on the far right of a periodic table, are uniquely unreactive with other elements. This property makes them well-suited for estimating past temperatures. By measuring the dissolved concentrations of noble gases in ancient groundwater, researchers at Columbia University's Lamont-Doherty Earth Observatory hope to determine how many degrees New Zealand warmed as it came out of the last ice age some 20,000 years ago.  In early June, a research team led by Martin Stute, a hydrologist with joint appointments at Lamont-Doherty and Barnard College, collected groundwater samples from a dozen wells on New Zealand's North and South Islands. I traveled with Stute and his colleagues Uwe Morgenstern and Mike Stewart from New Zealand's Institute of Geological and Nuclear Sciences (GNS) to do the sampling.

Elsewhere in New Zealand, Lamont-Doherty researchers have used surface exposure dating of glacial moraines in the Southern Alps to also reconstruct climate changes from the last ice age. Our pilot study aims to compare those results with our groundwater analysis to resolve an ongoing debate about how much warming occurred at low-latitudes and mid-latitudes in the southern hemisphere. Understanding the magnitude and timing of warming in the Southern Hemisphere at the end of the last ice age is important for better understanding global climate sensitivity.

Here's how our method works. Henry's law, a favorite equation of high school chemistry courses, equates the amount of dissolved gas in a fluid to its partial pressure multiplied by a temperature-dependent coefficient. Henry's law also represents the basic principle behind paleotemperature reconstructions from groundwater, a proxy scientists have used in paleoclimate research worldwide since the 1970s. By knowing the partial pressures (concentrations) of atmospheric gases, past temperature can be inferred from old groundwater since the concentrations of dissolved gases in groundwater are temperature-dependent. But, of course, many gases react with water or are used in biological processes, altering their concentrations over time and making them unreliable temperature indicators. Noble gases, which are inert, are unique: their dissolved concentrations in old groundwater are a conservative proxy for past mean annual temperature.

Seltzer is a senior in Columbia's Department of Earth and Environmental Sciences.