Dr. Larry Vardiman

• Technical Research Paper

  Numerical Simulations of Three Nor’easters with a Warm Atlantic Ocean

  March 28, 2012 from Answers Research Journal

  Analyses and numerical simulations were conducted on three recent nor’easters which formed on the East Coast of the United States to explore the effects of warmer-than-normal sea-surface temperatures.

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• Technical Research Paper

  Numerical Simulations of Hypercanes Charley and Fay in the Caribbean and the Gulf of Mexico over a Warm Ocean

  Feb. 29, 2012 from Answers Research Journal

  Two tropical cyclones were simulated with the NCAR WRF model to determine if warm sea-surface temperatures would cause them to intensify into hypercanes and follow similar storm tracks as the origin

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• Technical Research Paper

  A Well-Watered Land: Numerical Simulations of a Hypercyclone in the Middle East

  April 13, 2011 from Answers Research Journal

  A hypercyclone was simulated over the Arabian Sea to test enhanced precipitation over the Middle East and explain evidence for greater vegetation in the past.

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• Technical Research Paper

  Numerical Simulation of Precipitation in Yellowstone National Park with a Warm Ocean: Continuous Zonal Flow, Gulf of Alaska Low, and Plunging Western Low Case Studies

  Oct. 20, 2010 from Answers Research Journal

  Based on the likely four-fold increase in precipitation rate and doubling of the frequency of storms following the Genesis Flood, glaciers over a kilometer thick would have developed in a few hundred

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• Technical Research Paper

  Numerical Simulation of Precipitation in Yosemite National Park with a Warm Ocean: A Pineapple Express Case Study

  Feb. 17, 2010 from Answers Research Journal

  Based on the likely increase in precipitation rate and frequency of storms following the Genesis Flood, glaciers thousands of feet thick would have developed in a few hundred years.

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• Technical Research Paper

  Rapid Changes in Oxygen Isotope Content of Ice Cores

  April 1, 1997, pp. 52–60

  Oxygen isotopes in ice cores extracted from polar regions exhibit a decreasing trend in the ratio of the heavy to light isotopes from the beginning of the Ice Age to its end.

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