Snow Modeling and Observations at NOAA's National Operational
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An Evaluation of Snow Initializations in NCEP Global and Regional Forecasting Models
JUNE 2016 D A W S O N E T A L . 1885 An Evaluation of Snow Initializations in NCEP Global and Regional Forecasting Models NICHOLAS DAWSON,PATRICK BROXTON,XUBIN ZENG, AND MICHAEL LEUTHOLD Department of Atmospheric Sciences, The University of Arizona, Tucson, Arizona MICHAEL BARLAGE Research Applications Laboratory, Boulder, Colorado PAT HOLBROOK Idaho Power Company, Boise, Idaho (Manuscript received 13 November 2015, in final form 10 April 2016) ABSTRACT Snow plays a major role in land–atmosphere interactions, but strong spatial heterogeneity in snow depth (SD) and snow water equivalent (SWE) makes it challenging to evaluate gridded snow quantities using in situ measurements. First, a new method is developed to upscale point measurements into gridded datasets that is superior to other tested methods. It is then utilized to generate daily SD and SWE datasets for water years 2012–14 using measurements from two networks (COOP and SNOTEL) in the United States. These datasets are used to evaluate daily SD and SWE initializations in NCEP global forecasting models (GFS and CFSv2, both on 0.5830.58 grids) and regional models (NAM on 12 km 3 12 km grids and RAP on 13 km 3 13 km grids) across eight 28328 boxes. Initialized SD from three models (GFS, CFSv2, and NAM) that utilize Air Force Weather Agency (AFWA) SD data for initialization is 77% below the area-averaged values, on av- erage. RAP initializations, which cycle snow instead of using the AFWA SD, underestimate SD to a lesser degree. Compared with SD errors, SWE errors from GFS, CFSv2, and NAM are larger because of the ap- plication of unrealistically low and globally constant snow densities. -
Assessment of Snowfall Accumulation from Satellite and Reanalysis Products Using SNOTEL Observations in Alaska
Preprints (www.preprints.org) | NOT PEER-REVIEWED | Posted: 2 June 2021 doi:10.20944/preprints202106.0062.v1 Assessment of Snowfall Accumulation from Satellite and Reanalysis Products using SNOTEL Observations in Alaska Yang Song, Patrick D. Broxton, Mohammad Reza Ehsani, Ali Behrangi The University of Arizona, Department of Hydrology and Atmospheric Sciences Corresponding author: Ali Behrangi, [email protected] Abstract The combination of snowfall, snow water equivalent (SWE), and precipitation rate measurements from 39 Snow Telemetry (SNOTEL) sites in Alaska are used to assess the performance of various precipitation products from satellites, reanalysis, and rain gauges. Observation of precipitation from two water years (2018-2019) of the high resolution radar/rain gauge data (Stage IV) product was also utilized to add insights into scaling differences between various products. The outcomes were also used to assess two popular methods for rain gauge undercatch correction. It was found that SWE and precipitation measurements at SNOTELs, as well as precipitation estimates based on Stage IV data, are generally consistent and can provide a range in which other products can be assessed. Time-series of snowfall and SWE accumulation suggests that most of the products can capture snowfall events; however, differences exist in their accumulation. Reanalysis products tend to overestimate snow accumulation in the study area, while current combined passive microwave remote sensing products (i.e., IMERG-HQ) underestimate snowfall accumulation. We found that corrections factors applied to rain gauges are effective in improving their undercatch, especially for snowfall. However, no improvement in correlation is seen when correction factors are applied, and rainfall is still estimated better than snowfall. -
Download Gate.Html (Accessed on 20 April 2021)
remote sensing Article Assessment of Snowfall Accumulation from Satellite and Reanalysis Products Using SNOTEL Observations in Alaska Yang Song 1, Patrick D. Broxton 2, Mohammad Reza Ehsani 1 and Ali Behrangi 1,* 1 Department of Hydrology and Atmospheric Sciences, The University of Arizona, Tucson, AZ 85721, USA; [email protected] (Y.S.); [email protected] (M.R.E.) 2 School of Natural Resources and the Environment, The University of Arizona, Tucson, AZ 85721, USA; [email protected] * Correspondence: [email protected] Abstract: The combination of snowfall, snow water equivalent (SWE), and precipitation rate mea- surements from 39 snow telemetry (SNOTEL) sites in Alaska were used to assess the performance of various precipitation products from satellites, reanalysis, and rain gauges. Observation of precipita- tion from two water years (2018–2019) of a high-resolution radar/rain gauge data (Stage IV) product was also utilized to give insights into the scaling differences between various products. The outcomes were used to assess two popular methods for rain gauge undercatch correction. It was found that SWE and precipitation measurements at SNOTELs, as well as precipitation estimates based on Stage IV data, are generally consistent and can provide a range within which other products can be assessed. The time-series of snowfall and SWE accumulation suggests that most of the products can capture snowfall events; however, differences exist in their accumulation. Reanalysis products tended to overestimate snow accumulation in the study area, while the current combined passive microwave Citation: Song, Y.; Broxton, P.D.; remote sensing products (i.e., IMERG-HQ) underestimate snowfall accumulation. -
Snotel Representativeness in the Rio Grande Headwaters on the Basis of Physiographics and Remotely-Sensed Snow Cover Persistence
SNOTEL REPRESENTATIVENESS IN THE RIO GRANDE HEADWATERS ON THE BASIS OF PHYSIOGRAPHICS AND REMOTELY-SENSED SNOW COVER PERSISTENCE Noah P. Molotch1 and Roger C. Bales2 ABSTRACT Snowpack telemetry (SNOTEL) sites in and around the Rio Grande headwaters basin are located at the middle elevations of the watershed, in relatively dense vegetation, and toward the western boundary of the watershed. Based on 8 years of Advanced Very High Resolution Radiometer data (1995 – 2002), the snow cover persistence index value at the six SNOTEL sites ranged from 3.9 to 4.4 with an average 12% greater than the mean persistence of the watershed. Therefore, information from the sites does not capture the variability in snowpack accumulation and ablation processes across the watershed. Using elevation, western barrier distance, and vegetation density, a 32-node binary regression tree model explained 75% of the variability in average snow-cover persistence. Terrain classes encompassing the Lily Pond, Middle Creek, and Slumgullion SNOTEL sites represented 4.1, 6.4, and 4.0% of the watershed area, respectively. SNOTEL stations do not exist in the spatially extensive (e.g. 11% of the watershed) terrain classes located in the upper elevations above timberline. The results and techniques presented here will be useful for spatially distributed hydrologic analyses in that we have identified the physiographic conditions currently represented by SNOTEL stations (i.e. the snowpack regimes at which SWE estimation uncertainty can be determined). Further, we have outlined a statistically unbiased approach for designing future observation networks based on variability in physiographic attributes and snowpack processes. INTRODUCTION The most widely-used ground-based observations for evaluating, initializing, and updating grid element snowpack estimates currently come from the snowpack telemetry (SNOTEL) network. -
William Currier, Nic Wayand, & Jessica D. Lundquist
An Excel Based Module to Explore the Major Drivers of Snowmelt During Rain-On-Snow Flooding Events William Currier, Nic Wayand, & Jessica D. Lundquist *University of Washington, Mountain Hydrology Research, Civil and Environmental Engineering, Seattle, WA, USA Radiometer (CNR4) Introduction: A rain-on-snow flooding event is defined by extreme rain falling Data: Precipitation Gauge over a large extent of a snow-covered basin. Determining the contribution of I. Data to drive the model is taken from various locations: d) snowmelt during these events and determining the primary driver of the snow- 1. The Snoqualmie Pass research station (Figure 3) c) Wind Speed surface energy balance (Figure 1) is a critical question for flood forecasters and is a. Data is archived and available in real time1 2. Three National Resource Conservation Service (NRCS) not well understood due to sparse observations available over complex terrain. Air Temperature/ Existing snow energy balance models used for research are cumbersome to set up SNOTEL RH and run. Therefore, we have developed an Excel energy balance model that is a. Low through high elevation data is provided from the simple to set up, run and modify per the instructors goals. Our target audience is 2009 flood in the Snoqualmie Basin upper-level high school students or entry level undergraduates who have taken a II. Forcing data during different meteorological conditions is physics course and had some exposure to climatology. We include data taken from provided to run this model and includes: the Snoqualmie Pass research station (921 m) and three National Resource a. Air temperature Conservation Service SNOTEL stations in the Snoqualmie basin. -
4-H Weather and Climate Youth Learning Lab Leader's Guide
4-H Weather and Climate Youth Learning Lab Leader’s Guide 5351 • April 2019 Editors Molly Ward Science Educator Table of Contents Mountain Goat Instructional Design, LLC Bozeman, Montana Learning Lab Overview...................................3 Paul Lachapelle Introduction to Activities................................6 Associate Professor & Extension Community Activities Development Specialist; Department of Political Science; Local Government Center One: Weather Data............................................7 Montana State University Two: Weather and Climate Patterns.................... 12 Three: Weather and Climate Extremes................ 27 With contributions from: Four: Weather Forecasts................................... 31 Jasmine Carbajal MSU Extension FCS Agent, Hill County Five: CO2, Greenhouse Impacts and Climate....... 37 Six: Understanding Recent Climates Mary Louise Wood Wyoming State University Extension Educator, Through Tree Rings................................ 46 4-H/Youth Seven: Oceans, Ice and Modeling Climate........... 49 Shylea Wingard Eight: Where Does the Carbon Go?.................... 60 MSU Extension Agriculture and 4-H Agent, Nine: Weather and Climate Together, Hill County Now and in the Future............................ 64 Todd Kesner Director, MSU 4-H Center for Youth Development Katherine Jaeger The 4-H Experiential Learning Model Extension Field Specialist-Youth Outdoor Education, South Dakota State University provides the framework Mark Platten for this curriculum. Director, Teller County, Colorado -
Visibility Forecasts from the RUC20
5.10 Visibility Forecasts from the RUC20 Tracy Lorraine Smith*, Stanley G. Benjamin, and John M. Brown NOAA Research – Forecast Systems Laboratory Boulder, CO 80305 USA *Also affliliated with the Cooperative Institue for Research in the Atmosphere * email – [email protected] 1. Introduction 2002. The primary model changes in the RUC20 include a new Grell convective parameterization, At least five characteristics of the new 20-km explicit clouds using mixed phase microphysics, Rapid Update Cycle (RUC20, Benjamin et al. an update to the RUC/MM5 Reisner level-4 2002a, this volume), being implemented at NCEP mixed-phase microphysics developed jointly by in April 2002, should contribute to improvements NCAR and FSL, and new land-surface in visibility forecasts. These include higher processes. RUC20 also assimilates GOES horizontal and vertical resolution (from 40 km to cloud-top data to assist in the description of initial 20 km, 40 to 50 levels), improved versions of the cloud/hydrometeor fields. The smaller grid size MM5/RUC mixed-phase cloud microphysics and also allows the RUC20 to resolve smaller areas RUC land-surface schemes, assimilation of of clouds and precipitation, which should benefit GOES cloud information modifying RUC 1-h visibility diagnoses. A more accurate diurnal hydrometeor forecasts (Benjamin et al. 2002b), cycle with a more frequent call to the shortwave and an improved RUC visibility algorithm radiation module should also make a minor (Smirnova et al. 2000), which was originally contribution toward diagnosis of fog/low-level based on the Stoelinga-Warner method. clouds. Ongoing 3-h verification against METAR visibility observations is being conducted for forecasts The visibility field from the RUC is output from a from both the RUC2 (called RUC40 in this paper) visibility translation algorithm that uses near- and the RUC20 to assess the impact of the surface hydrometeor (cloud water, rain water, changes. -
A North American Hourly Assimilation and Model Forecast Cycle: the Rapid Refresh
APRIL 2016 B E N J A M I N E T A L . 1669 A North American Hourly Assimilation and Model Forecast Cycle: The Rapid Refresh STANLEY G. BENJAMIN,STEPHEN S. WEYGANDT,JOHN M. BROWN,MING HU,* CURTIS R. ALEXANDER,* TATIANA G. SMIRNOVA,* JOSEPH B. OLSON,* ERIC P. JAMES,* 1 DAVID C. DOWELL,GEORG A. GRELL,HAIDAO LIN, STEVEN E. PECKHAM,* 1 TRACY LORRAINE SMITH, WILLIAM R. MONINGER,* AND JAYMES S. KENYON* NOAA/Earth System Research Laboratory, Boulder, Colorado GEOFFREY S. MANIKIN NOAA/NWS/NCEP/Environmental Modeling Center, College Park, Maryland (Manuscript received 8 July 2015, in final form 8 December 2015) ABSTRACT The Rapid Refresh (RAP), an hourly updated assimilation and model forecast system, replaced the Rapid Update Cycle (RUC) as an operational regional analysis and forecast system among the suite of models at the NOAA/National Centers for Environmental Prediction (NCEP) in 2012. The need for an effective hourly updated assimilation and modeling system for the United States for situational awareness and related decision- making has continued to increase for various applications including aviation (and transportation in general), severe weather, and energy. The RAP is distinct from the previous RUC in three primary aspects: a larger geographical domain (covering North America), use of the community-based Advanced Research version of the Weather Research and Forecasting (WRF) Model (ARW) replacing the RUC forecast model, and use of the Gridpoint Statistical Interpolation analysis system (GSI) instead of the RUC three-dimensional variational data assimilation (3DVar). As part of the RAP development, modifications have been made to the community ARW model (especially in model physics) and GSI assimilation systems, some based on previous model and assimilation design innovations developed initially with the RUC. -
Water Year 2015 Summary of Climate, Hydrology & Snowpack
6th Annual Northwest Climate Conference November 4, 2015 Coeur d'Alene, Idaho Water Year 2015 Summary of Climate, Hydrology & Snowpack Observations Ron Abramovich Water Supply Specialist Snow Survey Boise, Idaho Water Year 2015 Summary of Climate, Hydrology & Snowpack Observations Abstract Water year 2015 was very unique in terms of climate variability in Idaho and the Pacific Northwest. We’ll discuss fall precipitation, the November arctic cold spell and how Christmas brought the best powder skiing conditions for the year. Development of the ‘Snow Drought’ and impacts from two Atmospheric River events that produced early runoff before the typical snowmelt runoff forecast period even started. A dry and warm March and April closed ski areas early and produced record high early irrigation demand. May’s rains provided some relief for southern Idaho irrigators. Record high June temperatures gave way to more reasonable July temperatures as the summer fire season grew in intensity. After the past unique year and several since 2011, everyone is looking and wondering what the winter of 2016 will bring to the Pacific Northwest. Water Year 2015 Summary of Climate, Hydrology & Snowpack Observations Abstract Water year 2015 was very unique in terms of climate variability in Idaho and the Pacific Northwest. We’ll discuss fall precipitation, the November arctic cold spell and how Christmas brought the best powder skiing conditions for the year. Development of the ‘Snow Drought’ and impacts from two Atmospheric River events that produced early runoff before the typical snowmelt runoff forecast period even started. A dry and warm March and April closed ski areas early and produced record high early irrigation demand. -
Evaluating Seasonal Orographic Precipitation in the Interior Western
SEPTEMBER 2017 J I N G E T A L . 2541 Evaluating Seasonal Orographic Precipitation in the Interior Western United States Using Gauge Data, Gridded Precipitation Estimates, and a Regional Climate Simulation XIAOQIN JING AND BART GEERTS Department of Atmospheric Science, University of Wyoming, Laramie, Wyoming YONGGANG WANG Department of Geosciences, Texas Tech University, Lubbock, Texas CHANGHAI LIU National Center for Atmospheric Research, Boulder, Colorado (Manuscript received 31 March 2017, in final form 12 July 2017) ABSTRACT There are several high-resolution (1–12 km) gridded precipitation datasets covering the interior western United States. This study cross validates seasonal orographic precipitation estimates from the Snowpack Telemetry (SNOTEL) network; the national hourly multisensor precipitation analysis Stage IV dataset (NCEP IV); four gauge-driven gridded datasets; and a 10-yr, 4-km, convection-permitting Weather Research and Forecasting (WRF) Model simulation. The NCEP IV dataset, which uses the NEXRAD network and precipitation gauges, is challenged in this region because of blockage and lack of low-level radar coverage in complex terrain. The gauge-driven gridded datasets, which statistically interpolate gauge measurements over complex terrain to better estimate orographic precipitation, are challenged by the highly heterogeneous, weather-dependent nature of precipitation in complex terrain at scales finer than can be resolved by the gauge network, such as the SNOTEL network. Gauge-driven gridded precipitation estimates disagree in areas where SNOTEL gauges are sparse, especially at higher elevations. The WRF simulation captures wintertime orographic precipitation distribution and amount well, and biases over specific mountain ranges are identical to those in an independent WRF simulation, suggesting that these biases are at least partly due to errors in the snowfall measurements or the gridding of these measurements. -
Weather and Climate Inventory National Park Service Sierra Nevada Network
National Park Service U.S. Department of the Interior Natural Resource Program Center Weather and Climate Inventory National Park Service Sierra Nevada Network Natural Resource Technical Report NPS/SIEN/NRTR—2007/042 ON THE COVER High alpine meadow in Yosemite National Park Photograph copyrighted by David Simeral Weather and Climate Inventory National Park Service Sierra Nevada Network Natural Resource Technical Report NPS/SIEN/NRTR—2007/042 WRCC Report 2007-17 Christopher A. Davey, Kelly T. Redmond, and David B. Simeral Western Regional Climate Center Desert Research Institute 2215 Raggio Parkway Reno, Nevada 89512-1095 June 2007 U.S. Department of the Interior National Park Service Natural Resource Program Center Fort Collins, Colorado The Natural Resource Publication series addresses natural resource topics that are of interest and applicability to a broad readership in the National Park Service and to others in the management of natural resources, including the scientific community, the public, and the National Park Service conservation and environmental constituencies. Manuscripts are peer-reviewed to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and designed and published in a professional manner. The Natural Resources Technical Reports series is used to disseminate the peer-reviewed results of scientific studies in the physical, biological, and social sciences for both the advancement of science and the achievement of the National Park Service mission. The reports provide contributors with a forum for displaying comprehensive data that are often deleted from journals because of page limitations. Current examples of such reports include the results of research that address natural resource management issues; natural resource inventory and monitoring activities; resource assessment reports; scientific literature reviews; and peer-reviewed proceedings of technical workshops, conferences, or symposia. -
An Investigation of Severe Weather Environments in Atmospheric Reanalyses Austin Taylor King
University of North Dakota UND Scholarly Commons Theses and Dissertations Theses, Dissertations, and Senior Projects January 2018 An Investigation Of Severe Weather Environments In Atmospheric Reanalyses Austin Taylor King Follow this and additional works at: https://commons.und.edu/theses Recommended Citation King, Austin Taylor, "An Investigation Of Severe Weather Environments In Atmospheric Reanalyses" (2018). Theses and Dissertations. 2251. https://commons.und.edu/theses/2251 This Thesis is brought to you for free and open access by the Theses, Dissertations, and Senior Projects at UND Scholarly Commons. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of UND Scholarly Commons. For more information, please contact [email protected]. AN INVESTIGATION OF SEVERE WEATHER ENVIRONMENTS IN ATMOSPHERIC REANALYSES by Austin Taylor King Bachelor of Science, University of Oklahoma, 2016 A Thesis Submitted to the Graduate Faculty of the University of North Dakota in partial fulfillment of the requirements for the degree of Master of Science Grand Forks, North Dakota May 2018 Copyright 2018 Austin King ii PERMISSION Title An Investigation of Severe Weather Environments in Atmospheric Reanalyses Department Atmospheric Sciences Degree Master of Science In presenting this thesis in partial fulfillment of the requirements for a graduate degree from the University of North Dakota, I agree that the library of this University shall make it freely available for inspection. I further agree that permission for extensive copying for scholarly purposes may be granted by the professor who supervised my thesis work or, in his absence, by the Chairperson of the department or the dean of the School of Graduate Studies.