Wickert, Andrew D.听1听;听Anderson, Robert S.听2听;听Mitrovica, Jerry X.听3
1听University of Colorado
2听University of Colorado
3听Harvard University
Glacial cycles modified North American river systems by drastically changing drainage basin areas, patterns of precipitation, and meltwater delivery to channels. We reconstruct drainage basins and river discharges in North America from 20,000 years ago to present by combining the ICE-5G ice sheet reconstruction [Peltier, 2004] with a state-of-the-art model of sea level that includes isostatic, gravitational, and rotational solid Earth response to changing ice and water loads [Mitrovica and Milne, 2003; Kendall et al., 2005] and a paleoclimate general circulation model [Liu et al., 2009]. We present the histories of these rapidly-evolving drainage systems, which are responsible for shaping the modern river networks of North America.
Kendall, R. A., J. X. Mitrovica, and G. A. Milne (2005), On post-glacial sea level--II. Numerical formulation and comparative results on spherically symmetric models, Geophysical Journal International, 161(3), 679-706.
锘縇iu, Z. et al. (2009), Transient simulation of last deglaciation with a new mechanism for Bolling-Allerod warming., Science, 325(5938), 310-4.
锘縈itrovica, J. X., and G. A. Milne (2003), On post-glacial sea level: I. General theory, Geophysical Journal International, 154(2), 253-267.
锘縋eltier, W. R. R. (2004), Global Glacial Isostasy and the Surface of the Ice-Age Earth: The ICE-5G (VM2) Model and GRACE, Annual Review of Earth and Planetary Sciences, 32(1), 111-149.