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Historical Derived DOF/DOT/LOGS - 771m CRU TS

This set of files includes downscaled historical estimates of decadal means of annual day of freeze or thaw (ordinal day of the year), and length of growing season (numbers of days, 0-365) for each decade from 1910 - 2006 (CRU TS 3.0) or 2009 (CRU TS 3.1) at at 771 x 771 meter spatial resolution. Each file represents a decadal mean of an annual mean calculated from mean monthly data.

Simple

Date (Publication)
2012-05-08
Credit
Matthew Leonawicz
Credit
Michael Lindgren
Credit
Tom Kurkowski
Credit
John Walsh
Credit
Scott Rupp
Status
Completed
Point of contact
  Scenarios Network for Alaska and Arctic Planning
Maintenance and update frequency
As needed
Theme
  • thaw
  • freeze
  • growing season
  • historical
  • modeled
Use constraints
License
Other constraints
https://creativecommons.org/licenses/by/4.0/
Spatial representation type
Grid
Distance
771  m
Metadata language
eng
Character set
UTF8
Topic category
  • Climatology, meteorology, atmosphere
Begin date
1900-01-15
End date
2009-12-31
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Supplemental Information

Day of freeze or thaw units are ordinal day 15-350 with the below special cases.

Day of Freeze (DOF)

0 = Primarily Frozen

365 = Rarely Freezes

Day of Thaw (DOT)

0 = Rarely Freezes

365 = Primarily Frozen

Length of Growing Season (LOGS)* is simply the number of days between the DOT and DOF

The spatial extent includes Alaska.

Each set of files originates from the Climatic Research Unit (CRU, http://www.cru.uea.ac.uk/ ) TS 3.0 or 3.1 dataset. TS 3.0 extends through December 2006 while 3.1 extends to December 2009.

Day of Freeze, Day of Thaw, Length of Growing Season calculations:

Estimated ordinal days of freeze and thaw are calculated by assuming a linear change in temperature between consecutive months. Mean monthly temperatures are used to represent daily temperature on the 15th day of each month. When consecutive monthly midpoints have opposite sign temperatures, the day of transition (freeze or thaw) is the day between them on which temperature crosses zero degrees C. The length of growing season refers to the number of days between the days of thaw and freeze.

This amounts to connecting temperature values (y-axis) for each month (x-axis) by line segments and solving for the x-intercepts. Calculating a day of freeze or thaw is simple. However, transitions may occur several times in a year, or not at all. The choice of transition points to use as the thaw and freeze dates which best represent realistic bounds on a growing season is more complex. Rather than iteratively looping over months one at a time, searching from January forward to determine thaw day and from December backward to determine freeze day, stopping as soon as a sign change between two months is identified, the algorithm looks at a snapshot of the signs of all twelve mean monthly temperatures at once, which enables identification of multiple discrete periods of positive and negative temperatures. As a result more realistic days of freeze and thaw and length of growing season can be calculated when there are idiosyncrasies in the data.

Unique resource identifier
EPSG:3338
Number of dimensions
2
Dimension name
Row
Dimension size
2557
Resolution
771  m
Dimension name
Column
Dimension size
4762
Resolution
771  m
Cell geometry
Area
Distribution format
  • GeoTIFF ( 1.0 )

OnLine resource
http://data.snap.uaf.edu/data/Base/AK_771m/historical/CRU_TS/Historical_Derived_DOF_DOT_LOGS_771m_CRU_TS ( WWW:LINK-1.0-http--link )
Hierarchy level
Dataset
Statement
SNAP downscaled data products are value added products that build off of other datasets that have been accepted by the scientific community as some of the highest quality climate data available.
File identifier
5eeefaa1-3e9e-4f01-94f6-e8f4fbbfc9c4 XML
Metadata language
English
Character set
UTF8
Date stamp
2023-10-26T12:15:17
Metadata standard name
ISO 19115:2003/19139
Metadata standard version
1.0
Point of contact
  Scenarios Network for Alaska and Arctic Planning
 
 

Overviews

overview

Spatial extent

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Keywords

freeze growing season historical modeled thaw

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