- #36
Xnn
- 555
- 0
Yes; the problem of deuterium-excess from Greenland ice cores is much more complex than for Antarctica.
Further progress should result from the use of isotopic ocean atmosphere
General Circulation Models to account for the complexity of topographic changes, source conditions and atmospheric circulation. They have, however, up to now, shown a very poor representation of the predicted characteristics of deuterium-excess in precipitation and clearly require additional work.
Nonetheless, these models are our best hope to account for sources of complexity,
such as the shifts of source locations. In addition, they can be used to investigate some of the implicit but important assumptions embedded in the simple models. With significant improvements, isotopic GCMs would be ideal tools to examine the properties of stable isotopes, including excess, in regions such as Greenland.
Further progress should result from the use of isotopic ocean atmosphere
General Circulation Models to account for the complexity of topographic changes, source conditions and atmospheric circulation. They have, however, up to now, shown a very poor representation of the predicted characteristics of deuterium-excess in precipitation and clearly require additional work.
Nonetheless, these models are our best hope to account for sources of complexity,
such as the shifts of source locations. In addition, they can be used to investigate some of the implicit but important assumptions embedded in the simple models. With significant improvements, isotopic GCMs would be ideal tools to examine the properties of stable isotopes, including excess, in regions such as Greenland.