TY - JOUR
T1 - Trends in twentieth-century U.S. snowfall using a quality-controlled dataset
AU - Kunkel, Kenneth E.
AU - Palecki, Michael A.
AU - Ensor, Leslie
AU - Hubbard, Kenneth G.
AU - Robinson, David
AU - Redmond, Kelly
AU - Easterling, David
PY - 2009
Y1 - 2009
N2 - A quality assessment of daily manual snowfall data has been undertaken for all U.S. long-term stations and their suitability for climate research. The assessment utilized expert judgment on the quality of each station. Through this process, the authors have identified a set of stations believed to be suitable for analysis of trends. Since the 1920s, snowfall has been declining in the West and the mid-Atlantic coast. In some places during recent years the decline has been more precipitous, strongly trending downward along the southern margins of the seasonal snow region, the southern Missouri River basin, and parts of the Northeast. Snowfall has been increasing since the 1920s in the lee of the Rocky Mountains, the Great Lakes - northern Ohio Valley, and parts of the north-central United States. These areas that are in opposition to the overall pattern of declining snowfall seem to be associated with specific dynamical processes, such as upslope snow and lake-effect snow that may be responding to changes in atmospheric circulation.
AB - A quality assessment of daily manual snowfall data has been undertaken for all U.S. long-term stations and their suitability for climate research. The assessment utilized expert judgment on the quality of each station. Through this process, the authors have identified a set of stations believed to be suitable for analysis of trends. Since the 1920s, snowfall has been declining in the West and the mid-Atlantic coast. In some places during recent years the decline has been more precipitous, strongly trending downward along the southern margins of the seasonal snow region, the southern Missouri River basin, and parts of the Northeast. Snowfall has been increasing since the 1920s in the lee of the Rocky Mountains, the Great Lakes - northern Ohio Valley, and parts of the north-central United States. These areas that are in opposition to the overall pattern of declining snowfall seem to be associated with specific dynamical processes, such as upslope snow and lake-effect snow that may be responding to changes in atmospheric circulation.
KW - ISWS
UR - http://www.scopus.com/inward/record.url?scp=62649170211&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=62649170211&partnerID=8YFLogxK
U2 - 10.1175/2008JTECHA1138.1
DO - 10.1175/2008JTECHA1138.1
M3 - Article
VL - 26
SP - 33
EP - 44
JO - Journal of Atmospheric and Oceanic Technology
JF - Journal of Atmospheric and Oceanic Technology
IS - 1
ER -