Canopy phenology of some mopane and miombo woodlands in eastern Zambia

rains. Plateau miombo exhibited the lowest range of seasonality in the tree layer, ranging from about Measurements of tree canopy closure and field-layer 40% to 60% closure over one complete seasonal reflectance were made in a series of plots in protected cycle. Phenology of the field layer, expressed as areas of eastern Zambia as part of a multiyear study the normalized diVerence vegetation index (NDVI), of savanna woodlands. The plots were located in closely followed that of the tree layer, although the the Luangwa Valley and adjacent plateaux, which field layer senesced earlier than trees, especially in contained a range of vegetation types found in plots with relatively low tree canopy closure. The southern Africa. The vegetation consisted of four relationship between tree-canopy closure and fieldbroad types: 1. plateau miombo woodland; layer NDVI was positive and statistically significant 2. valley miombo woodland; 3. scrub miombo for all sites of the study area, which suggests that woodland; and 4. scrub and woodland mopane. woody biomass and herbaceous biomass are related Hemispherical photographs of the tree layer positively in these savanna woodland ecosystems. provided measurements of tree canopy phenology in the diVerent vegetation plots. The most seasonal Key words. Canopy phenology, Zambezian woodlands, mopane woodland, miombo woodland, woodland type was mopane, where tree canopy closure ranged from about 15% at the end of the hemispherical photography, NDVI, Luangwa Valley, tree‐grass interactions. dry season to just over 60% during the peak of the

[1]  B. Walker,et al.  Interactions of woody and herbaceous vegetation in a southern African Savanna , 1985 .

[2]  C. Tucker Red and photographic infrared linear combinations for monitoring vegetation , 1979 .

[3]  A. J. Belsky,et al.  Stomatal responsiveness to changing light intensityincreases rain-use efficiency of below-crown vegetation in tropical savannas , 1995 .

[4]  S. Prince A model of regional primary production for use with coarse resolution satellite data , 1991 .

[5]  A. J. Belsky Tree/grass ratios in East African savannas: a comparison of existing models. , 1990 .

[6]  R. Webster A CATENA OF SOILS ON THE NORTHERN RHODESIA PLATEAU , 1965 .

[7]  F. Malaisse Phenology of the Zambezian Woodland Area with Emphasis on the Miombo Ecosystem , 1974 .

[8]  Samuel N. Goward,et al.  Transient Effects of Climate on Vegetation Dynamics: Satellite Observations , 1995 .

[9]  R. Scholes,et al.  An African Savanna: Synthesis of the Nylsvley Study. , 1993 .

[10]  Edward J. Milton,et al.  A portable multiband radiometer for ground data collection in remote sensing , 1980 .

[11]  Stephen D. Prince,et al.  The influence of canopy strata on remotely sensed observations of savanna-woodlands , 1997 .

[12]  J. Leonard,et al.  The Vegetation of Africa , 1984 .

[13]  C. S. Holling,et al.  STABILITY OF SEMI-ARID SAVANNA GRAZING SYSTEMS , 1981 .

[14]  Stephen D. Prince,et al.  Rainfall and foliar dynamics in tropical Southern Africa: Potential impacts of global climatic change on savanna vegetation , 1996 .

[15]  R. Webster,et al.  LAND CLASSIFICATION FOR MANAGEMENT PLANNING IN THE LUANGWA VALLEY OF ZAMBIA , 1969 .

[16]  J. Menaut,et al.  Influence of trees on above‐ground production dynamics of grasses in a humid savanna , 1995 .

[17]  B. Walker Ecological consequences of atmospheric and climate change , 1991 .

[18]  S. Azzali Interpretation of crop growth patterns by means of NDVI‐time series in Zambia , 1991 .

[19]  J. Weltzin,et al.  Savanna tree influence on understory vegetation and soil nutrients in northwestern Kenya , 1990 .