Archives: Articles

NOAA CLIMATE DATA STEWARDSHIP: PROGRESS THROUGH PARTNERSHIPS

Authors: Robert J. Leffler, Michael J. Brewer, Robert E. Livezey, Robert W. Reeves, Myron Berger, Timothy W. Owen, Karsten Shein
Volume: Volume 2007, No. 3, 2 Jun 2007
DOI: http://www.doi.org/10.46274/JoASC.2007.06.003
Abstract: Recent changes in the organizational structure of the National Oceanic and Atmospheric Administration (NOAA) have created an environment conducive to improved end-to-end agency climate data stewardship. Changes include the reintroduction of a climate services program into the National Weather Service (NWS) through the creation of a Climate Services Division (CSD) at the headquarters level, the creation of a NWS liaison at the National Climatic Data Center (NCDC), and the addition of six Regional Climate Centers as contractual support for NCDC. Action is being undertaken to mitigate deficiencies identified in the current surface weather and climate data collection, quality control, and dissemination process. Central to the effort in improving NOAA’s end-to-end data stewardship process is the strengthened partnerships and related coordination and collaboration between these different organizations. Strengthened partnerships, data policy changes, staff training in climate principles, and more effective operational practices ensure compliance with climate community needs and pay immediate dividends through increased data quality and data availability for all users. The evolution and changes noted above are documented. Future agency priorities for additional improvements that further protect the integrity of the nation’s climate record are also discussed.
Link: https://stateclimate.org/pdfs/journal-articles/2007_3-Leffler.pdf

RESEARCH DATA COLLECTION AT THE REYNOLDS CREEK EXPERIMENTAL WATERSHED

Authors: D. Marks, M. Seyfried, G. Flerchinger and A. Winstral
Volume: Volume 2007, No. 4, 2 Jun 2007
DOI: http://www.doi.org/10.46274/JoASC.2007.06.004
Abstract: To understand how variations in climate, land use, and land cover will impact water, ecosystem, and natural resources in snow-dominated regions, we must have access to long-term hydrologic and climatic databases. Data from watersheds that include significant human activities, such as grazing, farming, irrigation and urbanization, are critical for determining the signature of human induced changes on hydrologic processes and the water cycle. One of the primary components of effective watershed research is a sustained, long-term monitoring and measurement program. Such an effort was undertaken when the Reynolds Creek Experimental Watershed (RCEW) was added to the USDA Agricultural Research Service watershed program in 1960. The RCEW, a 239 km 2 drainage in the Owyhee Mountains near Boise, Idaho, has been continuously monitored since the early 1960's and continues to the present. The vision for RCEW as an outdoor hydrologic laboratory in which watershed re search would be supported by sustained, long-term monitoring of basic hydro-climatic parameters was described in 1965 in the first volume of Water Resources Research . Research at the RCEW continues to be supported by monitoring at 9 weirs, 21 primary and 4 secondary meteorological measurement stations, 24 precipitation stations, 8 snow courses, 5 snow study sites, 14 soil temperature profiles, 4 soil moisture profiles and 3 sub-surf ace hill-slope hydrology sites. These support a wide range of experimental investigations including snow hydrology and physics, cold season hydrology, water quality, model development and testing, water and carbon flux experiments, ecosystem processes studies, grazing effects, and mountain climate research. Active watershed manipulation allows research on fire ecology and hydrology, vegetation-climate interaction, watershed restoration, grazing and wildlife management, and invasive plants. All data are ingested into a computer database, and available to the public vi a both web-based and on-line ftp access.
Link: https://stateclimate.org/pdfs//journal-articles/2007_4-Marks.pdf

PAUL WAITE: 1918-2008

Authors: Harry J. Hillaker
Volume: Volume 2008, No. 1, 30 Jun 2008
DOI: http://www.doi.org/10.46275/JoASC.2008.06.001
Abstract: Paul J. Waite, long-time State Climatologist for Iowa, died at the age of 89 in Pittsfield, IL on April 28, 2008. Paul was born on June 21, 1918 in New Salem, IL. He graduated from New Salem High School in 1936 and received a Bachelor of Education in Science and Mathematics from Western State College in Macomb, IL in 1940. He taught and coached in several Illinois schools prior to entering the Air Force Meteorology Cadet Program at the University of Chicago in 1942. He served as a weather officer for the USAF from 1943 to 1946. He then served as a weather- briefer for the then US Weather Bureau in Chicago from 1948 to 1951. In 1951-1952 he served as a USAF meteorologist in Korea, then returned to work for the USWB in Kansas City. He was the USWB State Climatologist in Madison, WI from 1956- 1959, then took the same position in Des Moines, IA from 1959-1973.
Link: https://stateclimate.org/pdfs/journal-articles/2008_1-Hillaker.pdf

NWS FROST DEPTH OBSERVATION WITH LIQUID-IN PROBES PERFORMANCE: TWO-YEAR REVIEW

Authors: F. Adnan Akyuz, Mark Ewens, Radu Carcoana, Barbara Mullins
Volume: Volume 2009, No.1, 1 Jun 2009
DOI: http://www.doi.org/10.46275/JoASC.2009.06.001
Abstract: Performance of the liquid-in frost depth probe made in-house by the Grand Forks National Weather Service (NWS) Weather Forecast Office (W FO) is compared against soil temperature observations made by North Dakota Agricultural Weather Network (NDAWN) at the Fargo location for a two-year period from 2006-2007 to 2007-2008 winter seasons. While the liquid-in frost depth probe provided continuous frost depth observations, NDAWN soil temperature observations had to be interpolated between measurement points to determine the depth where the soil temperature was 0 °C (32 °F). In general, the trends of both observations matched almost identically; however, the magnitude of the depths varied with liquid-in frost depth probe consistently showing deeper frost depths than the NDAWN soil temperature observations.
Link: https://stateclimate.org/pdfs/journal-articles/2008_2-Akyuz.pdf

DAILY CLIMATE DATA QUALITY CONTROL PROCEDURES OF THE IOWA STATE CLIMATOLOGIST

Authors: Harry Hillaker, Karen Andsager
Volume: Volume 2009, No. 2, 1 Jun 2009
DOI: http://www.doi.org/10.46275/JoASC.2009.06.002
Abstract: The State Climatologist Office of the Iowa Department of Agriculture and Land Stewardship has been performing data entry and data quality control of National Oceanic and Atmospheric Administration daily climate data in Iowa since July 1, 1987. This process uses comprehensive, automated quality control tests based on standard instrumentation and observing practices and on standard climatological consistency. Inconsistencies flagged by these tests are manually resolved using a standard procedure based on information available from other sources and surrounding stations. The process then uses a manual spatial test to flag additional suspect values, which are also manually resolved using a standard procedure based on information available from other sources and surrounding stations. For example, for suspect values spotted in snowfall and snow depth spatial plots, visible satellite imagery may be consulted along with snowfall at neighboring stations to produce reasonable snowfall and snow depth estimates. This manually intensive process has produced a unique resource for comparison of manual quality control with automated processes, as well as analysis of Iowa climate.
Link: https://stateclimate.org/pdfs/journal-articles/2008_3-Hillaker.pdf

INTEGRATING THE NATURAL CLIMATE REGIME INTO MANAGEMENT PLANS FOR SWINE WASTEWATER LAGOONS

Authors: Charles L. Wax, Jonathan W. Pote, Michael E. Brown
Volume: Volume 2009, No. 3, 1 Jun 2009
DOI: http://www.doi.org/10.46275/JoASC.2009.06.003
Abstract: Disposal of wastewater from large-scale swine production facilities in the southern region of the U.S. is increasingly problematic as production facilities increase and regulations governing disposal become more restrictive. No-discharge systems are attractive or even mandatory for many producers. In such systems, wastewater is pumped from a storage lagoon when a certain level of storage is reached, and proper disposal depends on evaporation, infiltration into the soil, and on a crop's ability to utilize some nutrient such as nitrogen or phosphorus at that time. Under the control of climate in the region, lagoon levels rise during periods of precipitation while the soil becomes wet and the net water requirement of plants decreases, precluding irrigation. Wastewater volume is therefore typically high du ring winter and spring when pumping would be ecologically damaging, and low during summer and fall when conditions are more often suitable for successful land application. Consequently, at the moment of greatest need this type of disposal system is not operational, and spills or illegal discharges may occur. This study uses daily computer simulation over a 45-year period to test how well five management strategies could remedy this offset distribution of wastewater supply and demand. Pumping once each year on planned dates of the 15th of June, July, August, and September do successfully shift the time of necessary pumping out of the winter and spring and into the growing season. An annual September 15 th pumping of lagoons is recommended as the most efficient management plan for avoiding illegal overflows and emergency pumping at times when land application will not be successful.
Link: https://stateclimate.org/pdfs/journal-articles/2008_4-Wax.pdf

ALAN R. BENDER 1944-2008

Authors: Dennis Todey
Volume: Volume 2009, No. 4, 4 June 2009
DOI: http://www.doi.org/10.46275/JoASC.2009.06.004
Abstract: Alan R. Bender, 63, of Volga, S.D., died suddenly in Brookings on Wednesday, Aug. 27, 2008. In 1979 he became an engineer and assistant professor of agricultural engineering at SDSU and the following year he completed his master’s degree in agricultural engineering. In 1984 he was named acting director of the SDSU Water Resource Institute, a position he held until 1991. The previous year, he had been named an assistant professor and agricultural engineer in Extension and acting water quality coordinator. From 1991 to 2001 he was South Dakota’s state climatologist. His contributed significantly to the disciplinary knowledge base and helped pioneer many new processes through each of these positions; his professional achievements are too numerous to list.
Link: https://stateclimate.org/pdfs/journal-articles/2008_benderAl-obit-final-2008.pdf

MOLDING THE PIPELINE INTO A LOOP: THE PARTICIPATORY PROCESS OF DEVELOPING AGROCLIMATE, A DECISION SUPPORT SYSTEM FOR CLIMATE RISK REDUCTION IN AGRICULTURE

Authors: Norman E. Breuer, Clyde W. Fraisse, Peter E. Hildebrand
Volume: Volume 2009, No. 5, 7 October 2009
DOI: http://www.doi.org/10.46275/JoASC.2009.10.001
Abstract: We used a participatory approach for research, development, and dissemination of AgroClimate, a decision support system for climate risk reduction in agriculture. Feedback from stakeholders and dissemination of climate forecast technology were simultaneous outputs from interactions with potential end users. We describe the research and development process, including the use of Sondeos (a semi-structured, multidisciplinary team discussion process), focus groups, semi-structured interviews, web-surveys, on-line feedback and participation at farmer association meetings. Quality and quantity of feedback, cost, number of activities, and numbers of stakeholders reached were scaled for analysis. Radar diagrams were used to characterize the several research participatory methodologies used. Results showed that all methods were useful. The greatest quantity of feedback was obtained through Sondeos, interviews, and a web survey. The greatest quality of feedback came from the web survey, workshops, interviews and Sondeos. Dissemination of climate forecast technology and applications available on AgroClimate were greatest at farmer association meetings and lowest at workshops. All methods mentioned are appropriate loci for two-way translational science to occur. While disseminating climate information, feedback and new ideas from potential end users are obtained. Thus AgroClimate and many of the tools within it may be thought of as having been co-developed by scientists and stakeholders.
Link: https://stateclimate.org/pdfs/journal-articles/2009_Breuer-2009-JSC.pdf

THE TRANSITION OF THE BLANEY-CRIDDLE FORMULA TO THE PENMAN-MONTEITH EQUATION IN THE WESTERN UNITED STATES

Authors: Theodore W. Sammis, Junming Wang, David R. Miller
Volume: Volume 2011, No. 1, 21 Feb 2011
DOI: http://www.doi.org/10.46275/JoASC.2011.02.001
Abstract: This paper reviews the history of calculating “consumptive water use,” later termed evapotranspiration (Et), for plants in the western U.S. The Blaney-Criddle formula for monthly and seasonal consumptive water use was first developed for New Mexico in 1942 for limited crops. The formula was based on the input of monthly mean air temperature and an empirical monthly/seasonal coefficient. Subsequent changes improved the Blaney-Criddle formula by adding more weather and crop variables. The availability of data from automated weather stations, after about 1980, that measure more weather input variables has allowed the empirical Blaney-Criddle formula to be replaced by the mechanistic standardized Penman-Monteith equation with an appropriate crop coefficient to calculate Et. The Penman-Monteith equation calculates Et under non-stressed conditions and represents the maximum Et and associated yield of the crop.

Water rights in the western U.S. have historically, and continue to be, adjudicated using variations of the Blaney-Criddle formula. The Blaney-Criddle formula, derived in farmers’ fields under water stress conditions, calculates an Et that is most closely related to average county yields during the years the measurements were taken. But the empirical relationship and the originally derived coefficients are outdated and invalid for today’s agriculture production systems and should be replaced with the Penman-Monteith equation when adjudicating water rights.
Link: https://stateclimate.org/pdfs/journal-articles/2011_Sammis.A.11-working2A.pdf

CONTINENTAL WIND PATTERNS ASSOCIATED WITH COLORADO ALPINE DUST DEPOSITION: AN APPLICATION OF THE BLM/USFS RAWS NETWORK

Authors: Morgan Phillips, Nolan Doesken
Volume: Volume 2011, No. 2, 21 Jun 2011
DOI: http://www.doi.org/10.46275/JoASC.2011.06.001
Abstract: The winter and early spring of 2008-2009 brought an unusually high number of alpine dust deposition events to the Rocky Mountains of Colorado. The greatest dust accumulations were observed in the San Juan Mountains of southwestern Colorado. Significant dust accumulation was even observed along the Continental Divide in northern Colorado. The primary source for this dust has previously been identified as the Colorado Plateau. Analysis using the Hybrid Single Particle Lagrangian Integrated Trajectory (HYSPLIT) atmospheric trajectory model along with satellite imagery showed that dust from the 2009 events also originated from the Colorado Plateau, especially from areas in and around northeastern Arizona that were experiencing abnormally dry conditions that spring.

The study utilized data from the BLM/USFS Remote Automated Weather Station (RAWS) network in the southwestern U.S. to identify periods of high winds corresponding to documented Colorado dust events.The RAWS database, once considered to be brief and unsuitable as a climate resource, is quickly approaching 30 years of record and provides a valuable resource for application to various climate questions. Analysis of wind data from these RAWS sites during known dust events show that a minimum threshold wind velocity exists before dust storm generation occurs, and that this threshold velocity occurs from a southwesterly direction. Threshold velocity for the daily mean speed was found to be 15 mph and 44 mph for daily maximum gusts. Wind speeds for the study region were then evaluated for the period January through April for the past 20 years in an attempt to quantify and compare both mean daily wind speed and maximum daily wind gusts on a seasonal basis. A linear regression analysis showed correlation between the Southern Oscillation Index (SOI) and the frequency of these types of high wind periods in the RAWS database, particularly during winter months. This correlation was determined to be 0.46 for daily mean wind speeds and 0.56 for maximum daily wind gusts during the months of December through April. The correlation between periods of high winds and the SOI extends through the 20 years of wind data available for these weather stations.
Link: https://stateclimate.org/pdfs/journal-articles/2011_Phillips_2011_final_draft_mp.pdf