Cryospheric Climate Indicators: Greenness

Cryospheric Climate Indicators


Notice: The Sea Ice Index is updated monthly. Funding constraints prevent us from updating or developing the other Cryospheric Climate Indicators. Soil Temperatures, Snow Cover, and Greenness are shown as prototypes.

Greenness: Nascence

Nascence, or spring greenup, is marked by the day of year (plus or minus about 5 days) on which NDVI exceeds, for the first time, a threshold of 0.3. North of 55 deg N, this is usually between late May (DOY = 140) and the end of June (DOY = 180).

Average Nascence Day The average day greenup occurrs (to within about 10 days) over the period 1982 - 2001. From the Pathfinder data set.

Current Nascence Day Nascence day for the last growing season (to within about 16 days). From the MODIS data set. See Continuing the time series with MODIS data for discussion of differences with Pathfinder data.

Nascence Anomalies (Relative to 1982-2001 Mean)

Nascence Anomaly, First Five Years Pathfinder Data Minus Mean

 Mean 1982-1986 Nascence Minus Long Term Mean

Nascence Anomaly, Last Five Years Pathfinder Data Minus Mean

 Mean 1997-2001 Nascence Minus Long Term Mean

Notes: The anomaly images above show a trend toward earlier greenup (blue colors) over much of the Arctic in the last five years of our data record when compared with the first five years. In contrast to anomalies in SINDVI, however, there is considerable spatial variation. (The grey areas in the images above are where the threshold of 0.3 was not exceeded. Shield, bare rock, ice sheets, and areas largely covered by water have low or zero NDVI.) See Continuing the time series with MODIS data for discussion of why more recent MODIS data are not used.

Nascence (Day of Year), Regional Averages

Nascence (Day of Year) Anomaly, Regional Averages

Mean Regional Nascence DOY Output, Canada, Siberia, and Alaska Subsections Mean Regional Nascence DOY Anomaly, Canada, Siberia, and Alaska Subsections

Notes: Time series of nascence days (left) and anomalies (relative to the 1982-2001 mean, right) for regional subsets (red squares in the images). The nascence time series make evident that unlike SINDVI, the general advance in the day of spring greenup is not "in sync" everywhere. The dashed lines are data from MODIS. See Indicator Processing and Discussion for more information.

Nascence (Day of Year) Time Series, North Slope Subregions

Nascence (Day of Year) Anomaly Time Series, North Slope Subregions

Mean North Slope Subregions SINDVI Output Mean North Slope Subregions SINDVI Anomalies

Notes: The North Slope, Alaska, region was divided into subsections based on literature suggesting a different greening response for coastal versus inland tundra (see Discussion). Nascence for coastal tundra differs from inland higher elevation tundra by about 20 days. The anomaly series show that in spite of different greenness values, the two physiographical provinces are responding to changes similarly, although there is a suggestion that coastal tundra may be more sensitive to factors driving nascence than inland tundra.

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