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: NascenceNascence, 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).
Nascence Anomalies (Relative to 1982-2001 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.
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.
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. |