Sylvia Dee
0000-0002-2140-785X
Brown University
29 papers found
Refreshing results…
The dynamics of warming during the last deglaciation in high-elevation regions of Eastern Equatorial Africa
ENSO’s Response to Volcanism in a Data Assimilation‐Based Paleoclimate Reconstruction Over the Common Era
Last Millennium ENSO Diversity and North American Teleconnections: New Insights from Paleoclimate Data Assimilation
Resolving Long‐Term Variations in North Atlantic Tropical Cyclone Activity Using a Pseudo Proxy Paleotempestology Network Approach
Hot Air, Hot Lakes, or Both? Exploring Mid‐Holocene African Temperatures Using Proxy System Modeling
Assessing proxy system models of cave dripwater δ18O variability
Reduced lower Mississippi River discharge during the Medieval era
Response to Comment on “No consistent ENSO response to volcanic forcing over the last millennium”
Enhanced North American ENSO teleconnections during the Little Ice Age revealed by Paleoclimate Data Assimilation
The role of isotope‐enabled GCM complexity in simulating tropical circulation changes in high‐CO 2 scenarios
Lipid Biomarker Record Documents Hydroclimatic Variability of the Mississippi River Basin During the Common Era
Developing a coral proxy system model to compare coral and climate model estimates of changes in paleo‐ENSO variability
No consistent ENSO response to volcanic forcing over the last millennium
Subtropical Pacific Ocean Temperature Fluctuations in the Common Era: Multidecadal Variability and Its Relationship With Southwestern North American Megadroughts
La Niña-driven flooding in the Indo-Pacific warm pool during the past millennium
The Future of Reef Ecosystems in the Gulf of Mexico: Insights From Coupled Climate Model Simulations and Ancient Hot-House Reefs
WaxPSM: A Forward Model of Leaf Wax Hydrogen Isotope Ratios to Bridge Proxy and Model Estimates of Past Climate
Does volcanism cause warming or cooling?
Climate models can correctly simulate the continuum of global-average temperature variability
Evidence of Ice Age humans in eastern Beringia suggests early migration to North America
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