U.S. flag An official website of the United States government.
Official websites use .gov

A .gov website belongs to an official government organization in the United States.

Secure .gov websites use HTTPS

A lock ( ) or https:// means you've safely connected to the .gov website. Share sensitive information only on official, secure websites.

i

Half-century perspectives on North American spring snowline and snow cover association with the Pacific-North American teleconnection pattern

Supporting Files


Details

  • Journal Title:
    Climate Research
  • Personal Author:
  • NOAA Program & Office:
  • Description:
    Spring (MAM) snow coverage across North America (NA) has significantly declined during the last half-century (1967-2016), with possible linkages to changing behaviors in large-scale atmospheric circulation. In this study, we investigated relationships between intraseasonal, sub-continental NA snow cover characteristics and the Pacific-North American (PNA) teleconnection pattern, which quantifies longwave, ridge-trough fluctuations in the 500 hPa geopotential height (GPH) field over the Northern Hemisphere. Correlation and composite techniques were applied to analyze NA spring and intra-spring snow cover extent (SCE) and snowline (SL) associations with PNA index variations. Results show the PNA pattern to be significantly correlated to interannual SL and SCE during April and climatological spring, particularly over western NA. Anomalous PNA values (i.e. exceeding ±1 SD from the index mean) particularly influence transient snow in early/mid-spring. Composites of 500 hPa GPH and low-level air temperature fields suggest that both positive and negative March PNA index anomalies are linked with expansion of western and NA-wide snow cover, while positive (negative) April PNA anomalies yield retreat (advance) to varying magnitudes across sub-continental NA. Seasonal persistence of the PNA pattern is also an important factor in determining regional snow conditions, as negative PNA values in March-April favors above-normal total spring snow coverage, while positive PNA values in these months evoke a slight retreat (advance) that is dependent on negative (positive) phase persistence through May. This study provides additional insight into mid-tropospheric circulation connections to NA springtime snow cover during an era of rapid climate and environmental change.
  • Subjects:
  • Source:
    Clim Res 74:201-216
  • DOI:
  • Document Type:
  • Place as Subject:
  • Rights Information:
    CC BY
  • Compliance:
    Submitted
  • Download URL:
  • File Type:
    Filetype[PDF - 2.19 MB]
  • Collection(s):
  • Main Document Checksum:
    urn:sha256:ceedaba62f4203c43ec1f707201526c45c6aab3b4d8970c6392d5a7a91b98f19
ON THIS PAGE
 Found an issue?
Send us an email at:
The NOAA IR serves as an archival repository of NOAA-published products including scientific findings, journal articles, guidelines, recommendations, or other information authored or co-authored by NOAA or funded partners. As a repository, the NOAA IR retains documents in their original published format to ensure public access to scientific information.