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DATA OBSERVATIONS<br />

M<strong>as</strong>s Bal<strong>an</strong>ce<br />

The <strong>an</strong>nual bal<strong>an</strong>ce record shows a markedly positive trend from 1946–1988 period. The me<strong>an</strong><br />

<strong>an</strong>nual bal<strong>an</strong>ce for <strong>the</strong> 42-year period is 0.42 m/a, representing a total thickening of 17.5 m w.e or<br />

20 m in total ice thickness. From 1988–2005 m<strong>as</strong>s bal<strong>an</strong>ce ch<strong>an</strong>ged signific<strong>an</strong>tly <strong>an</strong>d h<strong>as</strong> been<br />

slightly negative averaging –0.17 m/a, a 3 m w.e. loss, or 3.3 meters of glacier thickness ch<strong>an</strong>ge<br />

(Figure 2). A comparison of surface height ch<strong>an</strong>ge along Profile 4 from 1993–2004 <strong>an</strong>d me<strong>an</strong><br />

surface bal<strong>an</strong>ce yield –3.5 m <strong>an</strong>d –2.7 m respectively. The next t<strong>as</strong>k in this research program is to<br />

determine <strong>the</strong> height ch<strong>an</strong>ges at survey location along additional profiles over <strong>an</strong> extended period,<br />

thus providing additional surface bal<strong>an</strong>ce data each year.<br />

m we<br />

20<br />

18<br />

16<br />

14<br />

12<br />

10<br />

8<br />

6<br />

4<br />

2<br />

0<br />

-2<br />

1946<br />

1949<br />

1952<br />

1955<br />

1958<br />

1961<br />

Juneau Icefield M<strong>as</strong>s Bal<strong>an</strong>ce<br />

Taku Cumulative bn Taku bn<br />

1964<br />

1967<br />

1970<br />

1973<br />

1976<br />

Year<br />

Figure 2. Annual <strong>an</strong>d cumulative m<strong>as</strong>s bal<strong>an</strong>ce of <strong>the</strong> Taku Glacier 1946–2005.<br />

With <strong>the</strong> distribution of <strong>an</strong>nual bal<strong>an</strong>ce more accurately mapped in <strong>the</strong> lower neve section of <strong>the</strong><br />

glacier b<strong>as</strong>ed on <strong>the</strong> 1998, 2003 <strong>an</strong>d 2004 combined snowpit <strong>an</strong>d probing me<strong>as</strong>urements, me<strong>an</strong><br />

<strong>an</strong>nual surface flux w<strong>as</strong> determined both for <strong>the</strong> glacier region above Profile 4 <strong>an</strong>d Profile 7,<br />

summing <strong>the</strong> products of <strong>the</strong> area observed between each 0.2 m m<strong>as</strong>s bal<strong>an</strong>ce interval <strong>an</strong>d <strong>the</strong><br />

<strong>an</strong>nual bal<strong>an</strong>ce for that interval. The surface flux accumulating above at Profile 4 w<strong>as</strong> calculated to<br />

be 5.5 × 10 8 m 3 a –1 , <strong>an</strong>d 1.90 × 10 8 m 3 a –1 above Profile 7.<br />

256<br />

1979<br />

1982<br />

1985<br />

1988<br />

1991<br />

1994<br />

1997<br />

2000<br />

2003<br />

2<br />

1.5<br />

1<br />

0.5<br />

0<br />

-0.5<br />

-1<br />

-1.5

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