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Judith Z. Drexler

Researcher at United States Geological Survey

Publications -  50
Citations -  1160

Judith Z. Drexler is an academic researcher from United States Geological Survey. The author has contributed to research in topics: Marsh & Peat. The author has an hindex of 17, co-authored 46 publications receiving 931 citations. Previous affiliations of Judith Z. Drexler include United States Forest Service & Cornell University.

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The Legacy of Wetland Drainage on the Remaining Peat in the Sacramento – San Joaquin Delta, California, USA

TL;DR: In this article, the authors studied the in situ effects of wetland drainage on the remaining peat in the Sacramento-San Joaquin Delta of California (hereafter, the Delta), where peat cores were retrieved from four drained, farmed islands and four relatively undisturbed, marsh islands.
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Wetland Accretion Rate Model of Ecosystem Resilience (WARMER) and Its Application to Habitat Sustainability for Endangered Species in the San Francisco Estuary

TL;DR: The Wetland Accretion Rate Model for Ecosystem Resilience (WARMER) is a 1-D model of elevation that incorporates both biological and physical processes of vertical marsh accretion as discussed by the authors.
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Accuracy and Precision of Tidal Wetland Soil Carbon Mapping in the Conterminous United States.

TL;DR: The assembled dataset showed that carbon density across the conterminous united states (CONUS) was normally distributed, with a predictable range of observations, and identified the simplest strategy, applying mean carbon density (27.0 kg C m−3), as the best performing strategy.
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Evapotranspiration rates and crop coefficients for a restored marsh in the Sacramento-San Joaquin Delta, California, USA

TL;DR: The surface renewal method was used to estimate evapotranspiration (ET) for a restored marsh on Twitchell Island in the Sacramento-San Joaquin Delta, California, USA as discussed by the authors.
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Widespread global peatland establishment and persistence over the last 130,000 y

TL;DR: It is shown that northern peatlands accumulate significant C stocks during warmer times, indicating their potential for C sequestration during the warming Anthropocene.