The case for more intense Eastern Pacific tropical cyclones arriving into southwestern North America during the Late Pleistocene: new geochronological and sedimentological evidence from central Baja California.
Jose Luis Antinao Rojas1, Marissa Rose Schorr1, Eric McDonald2, Tina M Niemi3, Kieran L. Bradley4, Jacqueline Jo Epperson5, Yahil Emmanuel Hernandez Salgado6, Genaro Martinez Gutierrez7 and Kam-Biu Liu8, (1)Indiana University Bloomington, Bloomington, IN, United States, (2)Desert Research Institute Reno, Reno, NV, United States, (3)University of Missouri-Kansas City, Department of Geosciences, Kansas City, MO, United States, (4)University of Missouri Kansas City, Kansas City, MO, United States, (5)Illinois State University, Geography, Geology, and the Environment, Bloomington, IL, United States, (6)Universidad Autónoma de Baja California Sur, Department of Earth Sciences, La Paz, BS, Mexico, (7)Universidad Autonoma de Baja California Sur, Department of Earth Sciences, La Paz, Mexico, (8)Louisiana State University, Oceanography and Coastal Sciences, Baton Rouge, LA, United States
