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Gonzalo Miguez-Macho  - - - 
Top co-authors See all
Hanqin Tian

472 shared publications

International Center for Climate and Global Change Research and School of Forestry and Wildlife Sciences, Auburn University, Auburn, AL 36849, USA

Alan Robock

285 shared publications

Department of Environmental Sciences; Rutgers University; New Brunswick NJ

Atul Jain

145 shared publications

Department of Atmospheric Sciences; University of Illinois at Urbana-Champaign; Urbana Illinois USA

Georgiy Lvovich Stenchikov

128 shared publications

King Abdullah University of Science and Technology; Physical Science and Engineering Division; Thuwal Kingdom of Saudi Arabia

Roy Rasmussen

109 shared publications

Research Application Lab, National Center for Atmospheric Research

Publication Record
Distribution of Articles published per year 
(2000 - 2018)
Publications See all
Article 0 Reads 1 Citation Reply to Pierret and Lacombe: Global controls on maximum rooting depths remain important. Ying Fan, Gonzalo Miguez-Macho, Esteban G Jobbágy, Robert B ... Published: 27 February 2018
Proceedings of the National Academy of Sciences, doi: 10.1073/pnas.1801899115
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Article 2 Reads 1 Citation A new moisture tagging capability in the Weather Research and Forecasting model: formulation, validation and application... Damián Insua-Costa, Gonzalo Miguez-Macho Published: 26 February 2018
Earth System Dynamics, doi: 10.5194/esd-9-167-2018
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A new moisture tagging tool, usually known as water vapor tracer (WVT) method or online Eulerian method, has been implemented into the Weather Research and Forecasting (WRF) regional meteorological model, enabling it for precise studies on atmospheric moisture sources and pathways. We present here the method and its formulation, along with details of the implementation into WRF. We perform an in-depth validation with a 1-month long simulation over North America at 20km resolution, tagging all possible moisture sources: lateral boundaries, continental, maritime or lake surfaces and initial atmospheric conditions. We estimate errors as the moisture or precipitation amounts that cannot be traced back to any source. Validation results indicate that the method exhibits high precision, with errors considerably lower than 1% during the entire simulation period, for both precipitation and total precipitable water. We apply the method to the Great Lake-effect snowstorm of November 2014, aiming at quantifying the contribution of lake evaporation to the large snow accumulations observed in the event. We perform simulations in a nested domain at 5km resolution with the tagging technique, demonstrating that about 30–50% of precipitation in the regions immediately downwind, originated from evaporated moisture in the Great Lakes. This contribution increases to between 50 and 60% of the snow water equivalent in the most severely affected areas, which suggests that evaporative fluxes from the lakes have a fundamental role in producing the most extreme accumulations in these episodes, resulting in the highest socioeconomic impacts.
Article 4 Reads 1 Citation The concurrence of atmospheric rivers and explosive cyclogenesis in the North Atlantic and North Pacific basins Jorge Eiras-Barca, Alexandre M. Ramos, Joaquim G. Pinto, Ric... Published: 22 January 2018
Earth System Dynamics, doi: 10.5194/esd-9-91-2018
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The explosive cyclogenesis of extratropical cyclones and the occurrence of atmospheric rivers are characteristic features of a baroclinic atmosphere, and are both closely related to extreme hydrometeorological events in the mid-latitudes, particularly on coastal areas on the western side of the continents. The potential role of atmospheric rivers in the explosive cyclone deepening has been previously analysed for selected case studies, but a general assessment from the climatological perspective is still missing. Using ERA-Interim reanalysis data for 1979–2011, we analyse the concurrence of atmospheric rivers and explosive cyclogenesis over the North Atlantic and North Pacific basins for the extended winter months (ONDJFM). Atmospheric rivers are identified for almost 80% of explosive deepening cyclones. For non-explosive cyclones, atmospheric rivers are found only in roughly 40% of the cases. The analysis of the time evolution of the high values of water vapour flux associated with the atmospheric river during the cyclone development phase leads us to hypothesize that the identified relationship is the fingerprint of a mechanism that raises the odds of an explosive cyclogenesis occurrence and not merely a statistical relationship. These new insights on the relationship between explosive cyclones and atmospheric rivers may be helpful to a better understanding of the associated high-impact weather events.
Article 4 Reads 4 Citations Evaluation of the moisture sources in two extreme landfalling atmospheric river events using an Eulerian WRF tracers too... Jorge Eiras-Barca, Francina Dominguez, Huancui Hu, Daniel Ga... Published: 22 December 2017
Earth System Dynamics, doi: 10.5194/esd-8-1247-2017
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A new 3-D tracer tool is coupled to the WRF model to analyze the origin of the moisture in two extreme atmospheric river (AR) events: the so-called Great Coastal Gale of 2007 in the Pacific Ocean and the Great Storm of 1987 in the North Atlantic. Results show that between 80 and 90% of moisture advected by the ARs, and a high percentage of the total precipitation produced by the systems have a tropical origin. The tropical contribution to precipitation is in general above 50% and largely exceeds this value in the most affected areas. Local convergence transport is responsible for the remaining moisture and precipitation. The ratio of tropical moisture to total moisture is maximized as the cold front arrives on land. Vertical cross sections of the moisture content suggest that the maximum in tropical humidity does not necessarily coincide with the low-level jet (LLJ) of the extratropical cyclone. Instead, the amount of tropical humidity is maximized in the lowest atmospheric level in southern latitudes and can be located above, below or ahead of the LLJ in northern latitudes in both analyzed cases.
Conference 10 Reads 0 Citations Tagging moisture sources with Eulerian and Lagrangian tracers: Application to an intense atmospheric river event. Vicente Perez-Muñuzuri, Jorge Eiras-Barca, Daniel Garaboa-Pa... Published: 08 November 2017
First International Electronic Conference on the Hydrological Cycle, doi: 10.3390/chycle-2017-04864
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Article 5 Reads 29 Citations Hydrologic regulation of plant rooting depth. Ying Fan, Gonzalo Miguez-Macho, Esteban G. Jobbágy, Robert B... Published: 18 September 2017
Proceedings of the National Academy of Sciences, doi: 10.1073/pnas.1712381114
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Plant rooting depth affects ecosystem resilience to environmental stress such as drought. Deep roots connect deep soil/groundwater to the atmosphere, thus influencing the hydrologic cycle and climate. Deep roots enhance bedrock weathering, thus regulating the long-term carbon cycle. However, we know little about how deep roots go and why. Here, we present a global synthesis of 2,200 root observations of >1,000 species along biotic (life form, genus) and abiotic (precipitation, soil, drainage) gradients. Results reveal strong sensitivities of rooting depth to local soil water profiles determined by precipitation infiltration depth from the top (reflecting climate and soil), and groundwater table depth from below (reflecting topography-driven land drainage). In well-drained uplands, rooting depth follows infiltration depth; in waterlogged lowlands, roots stay shallow, avoiding oxygen stress below the water table; in between, high productivity and drought can send roots many meters down to the groundwater capillary fringe. This framework explains the contrasting rooting depths observed under the same climate for the same species but at distinct topographic positions. We assess the global significance of these hydrologic mechanisms by estimating root water-uptake depths using an inverse model, based on observed productivity and atmosphere, at 30″ (∼1-km) global grids to capture the topography critical to soil hydrology. The resulting patterns of plant rooting depth bear a strong topographic and hydrologic signature at landscape to global scales. They underscore a fundamental plant-water feedback pathway that may be critical to understanding plant-mediated global change.