scispace - formally typeset
N

Naomi H. Naik

Researcher at Lamont–Doherty Earth Observatory

Publications -  43
Citations -  8347

Naomi H. Naik is an academic researcher from Lamont–Doherty Earth Observatory. The author has contributed to research in topics: Sea surface temperature & Ocean gyre. The author has an hindex of 31, co-authored 43 publications receiving 7795 citations. Previous affiliations of Naomi H. Naik include Columbia University & Vassar College.

Papers
More filters

Model Projections of an Imminent Transition to a More Arid Climate in

TL;DR: There is a broad consensus among climate models that this region will dry in the 21st century and that the transition to a more arid climate should already be under way, and the levels of aridity of the recent multiyear drought or the Dust Bowl and the 1950s droughts will become the new climatology of the American Southwest within a time frame of years to decades.
Journal ArticleDOI

Thermodynamic and Dynamic Mechanisms for Large-Scale Changes in the Hydrological Cycle in Response to Global Warming*

TL;DR: The mechanisms of changes in the large-scale hydrological cycle projected by 15 models participating in the Coupled Model Intercomparison Project phase 3 and used for the Intergovernmental Panel on Climate Change's Fourth Assessment Report are analyzed by computing differences between 2046 and 2065 and 1961 and 2000.
Journal ArticleDOI

Modeling of Tropical Forcing of Persistent Droughts and Pluvials over Western North America: 1856–2000*

TL;DR: The causes of persistent droughts and wet periods over western North America are examined in model simulations of the period from 1856 to 2000 as discussed by the authors, using either global sea surface temperature data as a lower boundary condition or observed data in just the tropical Pacific and computed the surface ocean temperature elsewhere with a simple ocean model.
Journal ArticleDOI

Is the Gulf Stream responsible for Europe's mild winters?

TL;DR: In this article, it was shown that the difference in winter temperatures across the North Atlantic, and the difference between western Europe and western North America, is essentially the same in these models whether or not the movement of heat by the ocean is accounted for.