Meredith Reitz is a Research Hydrologist for the USGS Water Resources Mission Area.
Dr. Meredith Reitz received a B.S. in Physics from Arizona State, with minors in Math, Astronomy, Political Science, and English. She completed a PhD in Physics at the University of Pennsylvania, where her advisor, Prof. Douglas Jerolmack, was a geomorphologist in the Earth and Environmental Science department. She then received a postdoctoral fellowship to work at Columbia University’s Lamont-Doherty Earth Observatory for two years. She has been with the USGS in Reston since August 2014, and works using remote sensing and ground-based data to estimate water cycle quantities of interest across the US.
Dr. Reitz’s work has generally focused on understanding the physical processes that drive dynamics of water and landscapes. Topics she has pursued have included methods for constraining remotely sensed evapotranspiration using ground-based data sources; the process and timescale of river channel movements on alluvial fans and braided rivers; the effect of vegetation on the stability and shape of sand dunes; and the interaction between river and tectonic systems. She has used a variety of methods in her research, including running physical experiments, analyzing time series images, topography, and remote sensing data with scripts written in Python (and ArcGIS/ ArcPy), MATLAB, and ImageJ, proposing new analytical treatments, and writing numerical models.
Current work
In her current research, Dr. Reitz is working toward estimating evapotranspiration, recharge, and runoff rates across the contiguous U.S., combining various methods and remote sensing as well as ground-based data sources.
She is a part of the team working on the Mississippi Alluvial Plain groundwater availability study. The project aims to improve our understanding the dynamics of groundwater availability in the water-stressed agricultural region of the Mississippi Alluvial Plain. Dr. Reitz’s work will further the water budget aspect of the project.
https://www2.usgs.gov/water/lowermississippigulf/map/
Dr. Reitz is also a PI on two Powell Center synthesis projects. The first one aims to better understand the utility of GRACE data (from the Gravity Recovery And Climate Experiment satellites) for remotely measuring water storage change, by bringing together GRACE data developers with researchers working on regional and national-scale groundwater modeling and field monitoring in a synthesis project. The second one aims to better understand the impacts of anthropogenic influence on global river basins, using remotely sensed and other data to develop a framework to better quantify the impacts of land use changes on ET and the water cycle.
Science and Products
A global synthesis of land-surface fluxes under natural and human-altered watersheds using the Budyko framework
A global synthesis of land-surface fluxes under natural and human-altered watersheds using the Budyko framework (COPY)
Mississippi Alluvial Plain (MAP): Water Availability Study
Integrating GRACE Satellite and Ground-based Estimates of Groundwater Storage Changes
Historical Evapotranspiration for the Conterminous U.S.
Urbanization Impacts on Evapotranspiration Across Various Spatio-temporal Scales
Monthly timescale quick-flow runoff maps for the conterminous U.S., 1895-2017
Combined remote sensing and water-balance evapotranspiration estimates (SSEBop-WB) for the conterminous United States
Annual estimates of recharge, quick-flow runoff, and ET for the contiguous US using empirical regression equations, 2000-2013
Ensemble estimation of historical evapotranspiration for the conterminous U.S.
Urbanization impacts on evapotranspiration across various spatio-temporal scales
HESS opinions: Beyond the long-term water balance: Evolving Budyko's supply–demand framework for the Anthropocene towards a global synthesis of land-surface fluxes under natural and human-altered watersheds
The use of national datasets to produce an average annual water budget for the Mississippi Alluvial Plain, 2000–13
Estimating quick-flow runoff at the monthly timescale for the conterminous United States
Combining remote sensing and water-balance evapotranspiration estimates for the conterminous United States
Annual estimates of recharge, quick-flow runoff, and ET for the contiguous U.S. using empirical regression equations
Non-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
Science and Products
- Science
A global synthesis of land-surface fluxes under natural and human-altered watersheds using the Budyko framework
Global hydroclimatic conditions have been significantly altered, over the past century, by anthropogenic influences that arise from warming global climate and also from local/regional anthropogenic disturbances. There has been never been an effort that has systematically analyzed how the spatio-temporal variability of land-surface fluxes vary in natural and human-altered watersheds globally. ThisA global synthesis of land-surface fluxes under natural and human-altered watersheds using the Budyko framework (COPY)
Global hydroclimatic conditions have been significantly altered, over the past century, by anthropogenic influences that arise from warming global climate and also from local/regional anthropogenic disturbances. There has been never been an effort that has systematically analyzed how the spatio-temporal variability of land-surface fluxes vary in natural and human-altered watersheds globally. ThisMississippi Alluvial Plain (MAP): Water Availability Study
The Mississippi Alluvial Plain is one of the most productive agricultural regions in the Nation and depends on groundwater for irrigation. The MAP area constitutes the third largest area of irrigated cropland in the United States. The area is approximately 29,000 square miles (19 million acres) and includes parts of the States of Missouri, Tennessee, Arkansas, Mississippi, and Louisiana.The U.S...Integrating GRACE Satellite and Ground-based Estimates of Groundwater Storage Changes
Groundwater storage depletion is a critical issue for many of the major aquifers in the U.S., particularly during intense droughts. The GRACE (Gravity Recovery and Climate Experiment) satellites launched in 2002, with sensors designed to measure changes in the Earth’s gravitational field at large spatial scales (≥ ~200,000 km2). These changes are primarily driven by changes in water storage on the... - Data
Historical Evapotranspiration for the Conterminous U.S.
This data release provides rasters of actual evapotranspiration (ET) at the Conterminous U.S. (CONUS) scale from October 1895 to September 2018. Data are provided at the annual and monthly time scales at 800 meter spatial resolution. The dataset was produced using ensemble estimation methods described in the associated journal article. The data release also includes associated datasets developed iUrbanization Impacts on Evapotranspiration Across Various Spatio-temporal Scales
The data in this release describe various aspects of the impacts of urbanization on evapotranspiration at local to global spatial scales. This data release is associated with the publication of these results in a concurrent journal article. Analyses in the journal article included comparisons between urban and non-urban ET in a variety of climate settings and spatial scales. Urbanization has beenMonthly timescale quick-flow runoff maps for the conterminous U.S., 1895-2017
This dataset includes 1 km resolution monthly timescale estimates of the contributions to the quick-flow runoff component of the water budget over the time period from 1895-2017. These estimates were developed with a regression for surface runoff data generated from a USGS-developed hydrograph separation program (PART) run on streamflow data from 1301 gaged watersheds as a function of surficial geCombined remote sensing and water-balance evapotranspiration estimates (SSEBop-WB) for the conterminous United States
This dataset includes 1km resolution monthly timescale estimates of evapotranspiration (ET) for the 2000-2015 timespan. These new SSEBop-WB estimates were developed by combining a previously published long-term annual average evapotranspiration map based on water balance constraints with the SSEBop remote sensing ET product (see Associated Items). The combination aims to leverage the advantages ofAnnual estimates of recharge, quick-flow runoff, and ET for the contiguous US using empirical regression equations, 2000-2013
This dataset includes 800m resolution long-term average estimates of evapotranspiration (ET), quick-flow runoff, and recharge within a closed water budget over the 2000-2013 time period and annual estimates for the individual years. It also includes other supporting data associated with the publication of these estimation methods in a concurrent journal article. These estimates were developed with - Publications
Ensemble estimation of historical evapotranspiration for the conterminous U.S.
Evapotranspiration (ET) is the largest component of the water budget, accounting for the majority of the water available from precipitation. ET is challenging to quantify because of the uncertainties associated with the many ET equations currently in use, and because observations of ET are uncertain and sparse. In this study, we combine information provided by available ET data and equations to prAuthorsMeredith Reitz, Ward E. Sanford, Samuel SaxeUrbanization impacts on evapotranspiration across various spatio-temporal scales
Urbanization has been shown to locally increase the nighttime temperatures creating urban heat islands, which partly arise due to evapotranspiration (ET) reduction. It is unclear how the direction and magnitude of the change in local ET due to urbanization varies globally across different climatic regimes. This knowledge gap is critical, both for the key role of ET in the energy and water balanceAuthorsAmirhossein Mazrooei, Meredith Reitz, Dingbao Wang, A. SankarasubramanianHESS opinions: Beyond the long-term water balance: Evolving Budyko's supply–demand framework for the Anthropocene towards a global synthesis of land-surface fluxes under natural and human-altered watersheds
Global hydroclimatic conditions have been substantially altered over the past century by anthropogenic influences that arise from the warming global climate and from local/regional anthropogenic disturbances. Traditionally, studies have used coupling of multiple models to understand how land-surface water fluxes vary due to changes in global climatic patterns and local land-use changes. We argue tAuthorsA. Sankarasubramanian, Dingbao Wang, Stacey A. Archfield, Meredith Reitz, Richard M Vogel, Amirhossein Mazrooei, Sudarshana MukhopadhyayaThe use of national datasets to produce an average annual water budget for the Mississippi Alluvial Plain, 2000–13
OverviewWater is a critically important resource for the Mississippi Alluvial Plain (MAP) region, supporting a multibillion-dollar agricultural industry. There are concerns that continued withdrawals of groundwater for irrigation may decrease future water supplies. The U.S. Geological Survey has a history of conducting research in the MAP region and recently began an effort to integrate multiple mAuthorsMeredith Reitz, Wade KressEstimating quick-flow runoff at the monthly timescale for the conterminous United States
The quantitative estimation of the quick-flow runoff component of streamflow is required for many hydrologic applications. Estimation at the monthly timescale and national spatial scale would be particularly useful for national water availability modeling. This paper reviews a sample of commonly used equations for quick-flow runoff, including several currently in use in continental-scale models. TAuthorsMeredith Reitz, Ward E. SanfordCombining remote sensing and water-balance evapotranspiration estimates for the conterminous United States
Evapotranspiration (ET) is a key component of the hydrologic cycle, accounting for ~70% of precipitation in the conterminous U.S. (CONUS), but it has been a challenge to predict accurately across different spatio-temporal scales. The increasing availability of remotely sensed data has led to significant advances in the frequency and spatial resolution of ET estimates, derived from energy balance pAuthorsMeredith Reitz, Gabriel Senay, Ward E. SanfordAnnual estimates of recharge, quick-flow runoff, and ET for the contiguous U.S. using empirical regression equations
This study presents new data-driven, annual estimates of the division of precipitation into the recharge, quick-flow runoff, and evapotranspiration (ET) water budget components for 2000-2013 for the contiguous United States (CONUS). The algorithms used to produce these maps ensure water budget consistency over this broad spatial scale, with contributions from precipitation influx attributed to eacAuthorsMeredith Reitz, Ward E. Sanford, Gabriel Senay, J. CazenasNon-USGS Publications**
Reitz, M., D.J. Jerolmack, and J.B. Swenson (2010), Flooding and flow path selection on alluvial fans and deltas, Geophysical Research Letters 37, doi: 10.1029/2009GL041985.Reitz, M., D.J. Jerolmack, R.L. Martin, and R.C. Ewing (2010), Barchan-parabolic dune pattern transition from vegetation stability threshold, Geophysical Research Letters 37, doi: 10.1029/2010GL044957.Jerolmack, D.J., M. Reitz, and R.L. Martin (2011), Sorting out abrasion in a gypsum dune field, J. Geophys. Res. 116, F02003, doi:10.1029/2010JF001821.Limare, A., M. Tal, M. Reitz, E. Lajeunesse, and F. Métivier (2011), Optical method for measuring bed topography and flow depth in an experimental flume, Solid Earth 2, 143-154, doi:10.5194/se-2-143-2011.Reitz, M., and D.J. Jerolmack (2012), Experimental alluvial fan evolution: channel dynamics, slope controls and shoreline growth. J. Geophys. Res.– Earth Surf. 117, F02021.Jerolmack, D.J., R.C. Ewing, F. Falcini, R.L. Martin, C. Masteller, C. Phillips, M. Reitz, and I. Buynevich (2012), Internal boundary layer model for the evolution of desert dune fields, Nature Geoscience5, 206–209, doi:10.1038/NGEO1381.Pickering, J.L, S.L. Goodbred, M.D. Reitz, T.R. Hartzog, D.R. Mondal, and M.S. Hossain (2013), Late Quaternary sedimentary record and Holocene channel avulsions of the Jamuna and Old Brahmaputra River Valleys in the Upper Bengal Delta Plain, Geomorphology 227: 123-136.Reitz, M., D.J. Jerolmack, E. Lajeunesse, A. Limare, O. Devauchelle, and F. Métivier (2014), Diffusive evolution of experimental braided rivers, Physical Review E 89, 052809.Litwin, K.L., M. Reitz, and D.J. Jerolmack (2014), Generalized sorting profiles of alluvial fans, Geophysical Research Letters, doi: 10.1002/2014GL060991.Reitz, M., J.L. Pickering, S.L. Goodbred Jr., C. Paola, M. Steckler, L. Seeber, and S.H. Akhter (2015), Effects of tectonic deformation and sea level on river path selection: theory and application to the Ganges-Brahmaputra-Meghna River Delta, JGR – Earth Surface.**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.