Michael F. Squires
National Oceanic and Atmospheric Administration
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Bulletin of the American Meteorological Society | 2012
Anthony Arguez; Imke Durre; Scott Applequist; Russell S. Vose; Michael F. Squires; Xungang Yin; Richard R. Heim; Timothy W. Owen
The National Oceanic and Atmospheric Administration (NOAA) released the 1981–2010 U.S. Climate Normals in July 2011, representing the latest decadal installment of this long-standing product line. Climatic averages (and other statistics) of temperature, precipitation, snowfall, and numerous derived quantities were calculated for ~9,800 stations operated by the U.S. National Weather Service (NWS). They include estimated normals, or “quasi normals,” for approximately 2,000 active short-record stations such as those in the U.S. Climate Reference Network. The 1981–2010 installment features several new products and methodological enhancements: 1) state-of-the-art temperature homogenization at the monthly scale, 2) extensive utilization of quality-controlled daily climate data, 3) new statistical approaches for calculating daily temperature normals and heating and cooling degree days, and 4) a comprehensive suite of precipitation, snowfall, and snow depth statistics. This paper provides a general overview of th...
Journal of Applied Meteorology and Climatology | 2013
Imke Durre; Michael F. Squires; Russell S. Vose; Xungang Yin; Anthony Arguez; Scott Applequist
AbstractThe 1981–2010 “U.S. Climate Normals” released by the National Oceanic and Atmospheric Administration’s (NOAA) National Climatic Data Center include a suite of monthly, seasonal, and annual statistics that are based on precipitation, snowfall, and snow-depth measurements. This paper describes the procedures used to calculate the average totals, frequencies of occurrence, and percentiles that constitute these normals. All parameters were calculated from a single, state-of-the-art dataset of daily observations, taking care to produce normals that were as representative as possible of the full 1981–2010 period, even when the underlying data records were incomplete. In the resulting product, average precipitation totals are available at approximately 9300 stations across the United States and parts of the Caribbean Sea and Pacific Ocean islands. Snowfall and snow-depth statistics are provided for approximately 5300 of those stations, as compared with several hundred stations in the 1971–2000 normals. T...
Bulletin of the American Meteorological Society | 2014
Michael F. Squires; Jay H. Lawrimore; Richard R. Heim; David A. Robinson; Mathieu R. Gerbush; Thomas Estilow
This paper describes a new snowfall index that quantifies the impact of snowstorms within six climate regions in the United States. The regional snowfall index (RSI) is based on the spatial extent of snowfall accumulation, the amount of snowfall, and the juxtaposition of these elements with population. Including population information provides a measure of the societal susceptibility for each region. The RSI is an evolution of the Northeast snowfall impact scale (NESIS), which NOAAs National Climatic Data Center began producing operationally in 2006. While NESIS was developed for storms that had a major impact in the Northeast, it includes all snowfall during the lifetime of a storm across the United States and as such can be thought of as a quasi-national index that is calibrated to Northeast snowstorms. By contrast, the RSI is a regional index calibrated to specific regions using only the snow that falls within that region. This paper describes the methodology used to compute the RSI, which requires re...
Bulletin of the American Meteorological Society | 2012
Scott Applequist; Anthony Arguez; Imke Durre; Michael F. Squires; Russell S. Vose; Xungang Yin
The 1981–2010 U.S. Climate Normals released by the National Oceanic and Atmospheric Administrations (NOAA) National Climatic Data Center (NCDC) include a suite of descriptive statistics based on hourly observations. For each hour and day of the year, statistics of temperature, dew point, mean sea level pressure, wind, clouds, heat index, wind chill, and heating and cooling degree hours are provided as 30-year averages, frequencies of occurrence, and percentiles. These hourly normals are available for 262 locations, primarily major airports, from across the United States and its Pacific territories. We encourage use of these products specifically for examination of the diurnal cycle of a particular variable, and how that change may shift over the annual cycle.
Bulletin of the American Meteorological Society | 2015
Imke Durre; Michael F. Squires
AbstractAre we going to have a white Christmas? That is a question that scientists at the National Oceanic and Atmospheric Administration (NOAA) receive each autumn from members of the media and general public. NOAA personnel typically respond by way of a press release and map depicting the climatological probability of observing snow on the ground on 25 December at stations across the contiguous United States. This map has become one of the most popular applications of NOAA’s 1981–2010 U.S. Climate Normals.The purpose of this paper is to expand upon the annual press release in two ways. First, the methodology for empirically calculating the probabilities of snow on the ground is documented. Second, additional maps describing the median snow depth on 25 December as well as the probability and amount of snowfall are presented. The results are consistent with a climatologist’s intuitive expectations. In the Sierras, Cascades, the leeward side of the Great Lakes, and northern New England, snow cover is a nea...
Geophysical Research Letters | 2013
Anthony Arguez; Thomas R. Karl; Michael F. Squires; Russell S. Vose
Archive | 2009
Michael F. Squires; Jay H. Lawrimore; Richard R. Heim; David A. Robinson; Mathieu R. Gerbush; Tom Estilow; Christopher Eugene Tabor; Anna M. Wilson
Geophysical Research Letters | 2013
Anthony Arguez; Thomas R. Karl; Michael F. Squires; Russell S. Vose
93rd American Meteorological Society Annual Meeting | 2013
Michael F. Squires
Archive | 2010
Jay H. Lawrimore; Michael F. Squires; David A. Robinson