Chrystaline polar ice has ample space between its molecules of water to trap chemical impurities and gases in the form of "fossil air" which provides a direct measurement of past atmospheres. It is these chemical impurities and gases that not only allow us to look at paleo-atmospheres, but to also provide a reliable chronology in which they occurred as well. Many of them are not only annual indicators but seasonal indicators as well.
The primary paleoclimate indicators measured in ice cores include stable isotopic ratios of the ice lattice and stable isotopes of the trapped gases as well. Some are soluble (NHO3, HCl, H2O2, NH3) and insoluble cations such as NH4+, Ca2+, Mg2+ and anions such as NO3-, ClSO4^2-, electrical conductivity and cosmogenic isotopes. Dust and pollen are also indicators as well.
The intent of this thread is to look into each of these climate indicators and how we are able to understand what they reveal.
The primary paleoclimate indicators measured in ice cores include stable isotopic ratios of the ice lattice and stable isotopes of the trapped gases as well. Some are soluble (NHO3, HCl, H2O2, NH3) and insoluble cations such as NH4+, Ca2+, Mg2+ and anions such as NO3-, ClSO4^2-, electrical conductivity and cosmogenic isotopes. Dust and pollen are also indicators as well.
The intent of this thread is to look into each of these climate indicators and how we are able to understand what they reveal.