48 research outputs found
Diverging climate trends in Mongolian taiga forests influence growth and regeneration of Larix sibirica
Central and semiarid north-eastern Asia was subject to twentieth century warming far above the global average. Since forests of this region occur at their drought limit, they are particularly vulnerable to climate change. We studied the regional variations of temperature and precipitation trends and their effects on tree growth and forest regeneration in Mongolia. Tree-ring series from more than 2,300 trees of Siberian larch (Larix sibirica) collected in four regions of Mongoliaâs forest zone were analyzed and related to available weather data. Climate trends underlie a remarkable regional variation leading to contrasting responses of tree growth in taiga forests even within the same mountain system. Within a distance of a few hundred kilometers (140â490Â km), areas with recently reduced growth and regeneration of larch alternated with regions where these parameters remained constant or even increased. Reduced productivity could be correlated with increasing summer temperatures and decreasing precipitation; improved growth conditions were found at increasing precipitation, but constant summer temperatures. An effect of increasing winter temperatures on tree-ring width or forest regeneration was not detectable. Since declines of productivity and regeneration are more widespread in the Mongolian taiga than the opposite trend, a net loss of forests is likely to occur in the future, as strong increases in temperature and regionally differing changes in precipitation are predicted for the twenty-first century
Das Arteninventar der Avifauna der Mongolei während einer Nord-Sßd-Durchquerung 1997
Here we present a detailed report on bird biodiversity of ecosystems along a North-South transect through Mongolia in 1997whic h serves as a guideline for further research projects and training for students in all Mongolian vegetation zones from northern steppes to southern deserts.
Two hundred fifty-five bird species were observed between 21st of July and 10th of August 1997. The main study sites were located in the North the Selenge-Orchon-basin with meadows and dune woodlands 15 km southern from Suchbaatar, the Middle Gobi-Aimag with desert steppes and sajrs (covered with Ulmus pumila) and in the Bordzongijn-gobi in the South including a landscape mosaic of desert and semidesert habitats.
Quantitative data of all observations regarding bird communities, population density, reproduction, ecology and taxonomy are summarized. The following bird families were noticed: Gaviidae (1), Podicipedidaa (4), Phalacrocoracidae (1), Ardeidae (1), Ciconiidae (1), Anatidae (21), Accipitridae (19), Falconidae (8),Phasianidae (2), Gruidae (1), Rallidae (6), Otidae (1), Charadriidae (6), Recurvirostridae (2), Scolopacidae (23), Laridae (6), Pteroclidae (1), Columbidae (6), Cuculidae (2), Strigidae (4), Caprimulgidae (1), Apodidae (3), Alcedinidae (1) Upupidae (1), Picidae (6), Hirundinidae (5), Alaudidae (7), Motacillidae (12), Troglodytidae (1), Prunellidae (3), Turdidae (21), Sylvidae (16), Muscicapidae (4), Aegithalidae (1), Paridae (5), Sittidae (1), Certhidae (1), Remizidae (1), Oriolidae (1), Laniidae (5), Corvidae (10), Sturnidae (3), Passeridae (5), Fringillidae (10), and Emberizidae (15)
Equations for estimating the above-ground biomass of Larix sibirica in the forest-steppe of Mongolia
Climate effects on vegetation vitality at the treeline of boreal forests of Mongolia
In northern Mongolia, at the southern boundary of the Siberian boreal forest
belt, the distribution of steppe and forest is generally linked to climate
and topography, making this region highly sensitive to climate change and
human impact. Detailed investigations on the limiting parameters of forest
and steppe in different biomes provide necessary information for
paleoenvironmental reconstruction and prognosis of potential landscape
change. In this study, remote sensing data and gridded climate data were
analyzed in order to identify main distribution patterns of forest and steppe
in Mongolia and to detect environmental factors driving forest development.
Forest distribution and vegetation vitality derived from the normalized
differentiated vegetation index (NDVI) were investigated for the three types
of boreal forest present in Mongolia (taiga, subtaiga and forestâsteppe),
which cover a total area of 73âŻ818âŻkm2. In addition to the
forest type areas, the analysis
focused on subunits of forest and nonforested areas at the upper and lower
treeline, which represent ecological borders between vegetation types.
Climate and NDVI data were analyzed for a reference period of 15Â years from
1999 to 2013.
The presented approach for treeline delineation by identifying representative
sites mostly bridges local forest disturbances like fire or tree cutting.
Moreover, this procedure provides a valuable tool to distinguish the
potential forested area. The upper treeline generally rises from 1800âŻm
above sea level (a.s.l.) in the northeast to 2700âŻmâŻa.s.l. in the south.
The lower treeline locally emerges at 1000âŻmâŻa.s.l. in the northern taiga
and rises southward to 2500âŻmâŻa.s.l. The latitudinal gradient of both
treelines turns into a longitudinal one on the eastern flank of mountain
ranges due to higher aridity caused by rain-shadow effects. Less productive
trees in terms of NDVI were identified at both the upper and lower treeline
in relation to the respective total boreal forest type area. The mean growing
season temperature (MGST) of 7.9â8.9âŻÂ°C and a minimum MGST of
6âŻÂ°C are limiting parameters at the upper treeline but are
negligible for the lower treeline. The minimum of the mean annual
precipitation (MAP) of 230â290âŻmmâŻyrâ1 is a limiting parameter at the
lower treeline but also at the upper treeline in the forestâsteppe ecotone.
In general, NDVI and MAP are lower in grassland, and MGST is higher compared
to the corresponding boreal forest. One exception occurs at the upper
treeline of the subtaiga and taiga, where the alpine vegetation consists of
mountain meadow mixed with shrubs. The relation between NDVI and climate data
corroborates that more precipitation and higher temperatures generally lead
to higher greenness in all ecological subunits. MGST is positively correlated
with MAP of the total area of forestâsteppe, but this correlation turns
negative in the taiga. The limiting factor in the forestâsteppe is the
relative humidity and in the taiga it is the snow cover distribution. The
subtaiga represents an ecological transition zone of approximately
300âŻmmâŻyrâ1 precipitation, which occurs independently from the MGST.
Since the treelines are mainly determined by climatic parameters, the rapid
climate change in inner Asia will lead to a spatial relocation of tree communities, treelines and
boreal forest types. However, a direct deduction of future tree vitality,
forest composition and biomass trends from the recent relationships between
NDVI and climate parameters is challenging. Besides human impact, it must
consider bio- and geoecological issues like, for example, tree rejuvenation,
temporal lag of climate adaptation and disappearing permafrost