Hyltemossa
General
The site Hyltemossa was established in 2014 in a 30 year old
managed spruce forest in southern Sweden.
The site hosts a combined atmosphere and ecosystem station.
Data download
Data from Hyltemossa can be downloaded from the ICOS Carbon Portal.ICOS Level2 data from the Atmosphere Station (GHG concentrations, air temperature, wind). ICOS Level2 data from the Ecosystem Station (flux data, meteorological data, soil meteorological variables, ancillary data)
Location
Hyltemossa is located a few kilometers south of Perstorp,
in northwestern Skåne ( 56°06′N,
13°25′E, 115 m asl).
Contact
The site is run by station PI Michal Heliasz at
Lund University.
Station principal investigator Michal Heliasz. | Research engineer Tobias Biermann. |
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You are welcome!
ICOS Sweden invites other research groups to use the infrastructure.
Please fill in our
web form.
Geology and Soil
The underlying bedrock at the site, found in a depth from 20 - 50 m, is
composed mainly from acidic intrusion rock such as Granite with some
limited occurrence of a younger ultrabasic rock such as Gabbro.
Quaternary deposits at the center of Hyltemossa Site are dominated by sandy till surrounded by glaciofluvial sediments. Occasionally fen peat and to a small extend crystalline rock and boulders can be found.
Soil at the site is classified as Cambisol with a shallow organic horizon, a transition to Podsol can be found in certain areas. Stones in various sizes are found frequently and in some areas influence of groundwater is obvious in 1 m depth.


Vegetation
The site around the tower is dominated by Norway spruce
(Picea abies) with a small fraction of birch trees
(Betula sp.) and single occurrence of Scots pine
(Pinus sylvestris). Understorey vegetation is sparse.
The forest floor is mainly covered by a thick moss layer.
The forest is owned and managed by Gustafsborg Säteri AB (www.gustafsborg.se). The management turnover rate is 50 years, with an estimated growth of 34 m within 100 years. The site experienced storm damage in 1981, was clear-cut in 1982 and replanted in 1983 with 3300 trees per hectare. The forest was cleaned in 1998 and 2005 and thinned in 2009 and 2013. At the present time the forest stand is 19 m tall and holds around 190 m3 per hectare (excluding branches, stumps and roots).
Click here to see a satellite image time lapse 1984-2016 on Google Earth Engine.


Climate
Data for the 1961-1990 climatological normal from the close by
SMHI station Ljungbyhed characterizes the climate as a Cfb-climate
(after Köppen), i.e. humid temperate with mild summers and
mild winters. Mean annual air temperature for Ljungbyhed is 7°C
and mean annual precipitation sums up to 830 mm.



ICOS measurements
All related, continuous, automatic measurements are listed below in alphabetical order.
The measurements are carried out either on the 150 m high tower, at the earth
surface, or in a soil pit and on a tree in one of the four continuous measurement points
located around the tower. All measurements are
carried out within a distance of about 200 m of the tower.
Variable | Measurement height (m) | |
air pressure | ||
air temperature | 27 | |
profile | 1, 4, 9, 14, 19, 24, 30, 40, 55, 70, 85, 100, 125, 148 | |
flux system | 27 | |
carbon dioxide (CO2) | profile | 1, 4, 9, 14, 19, 24, 30, 40, 55, 70, 85, 100, 125, 148 |
flux system | 27 | |
atmospheric system | 30, 70, 150 | |
carbon monoxide (CO) | atmospheric system | 30, 70, 150 |
ground water level | 4x, close to each soil profile | |
methane (CH4) | atmospheric system | 30, 70, 150 |
PAR | 4 transects in the canopy with each 4 sensors | 1 |
incoming and outgoing | 50 | |
diffuse and total incoming | 150 | |
precipitation | 1.5 | |
snow depth | ||
soil heat flux | 4x, together with each soil profile | -0.05 |
soil moisture | 4 profiles | 0 to -0.06 (vertical), -0.05, -0.1, -0.3, -1.0 |
soil temperature | 4 profiles | -0.02, -0.05, -0.1, -0.3, -1.0 |
solar radiation | incoming | 150 |
incoming and outgoing | 50 | |
sunshine duration | 150 | |
surface temperature | target temperature | |
terrestrial radiation | incoming and outgoing | 50 |
tree temperature | 4 spruce with 3 levels, and 4 sensors at each level (facing N, E, S, and W) | ∼3, ∼9, ∼15 |
water vapour | 27 | |
profile | 1, 4, 9, 14, 19, 24, 30, 40, 55, 70, 85, 100, 125, 148 | |
flux system | 27 | |
atmospheric system | 30, 70, 150 | |
wind vector | flux system | 27 |
Collaborations
As an infrastructure we are welcoming other research groups
to carry out their projects at our station. Actually, we have
three other projects that have joined at the Hyltemossa station:
Please click on an individual project to get more information.
Facilities
Hyltemossa Station has a main house and a workshop building.
The main house is equipped with a classroom, kitchen, office, four bedrooms
and and two bathrooms. It provides the possibility to hold small meetings or
courses for up to 14 participants and an opportunity for overnight stay
for up to ten persons.



Publications (peer-reviewed articles and theses)
-
2018
- Menegat, A., Milberg, P., Nilsson, A.T.S., Andersson, L. and Vico G. (2018): Soil water potential and temperature sum during reproductive growth control seed dormancy in Alopecurus myosuroides Huds. Ecol Evol., 8:7186-7194, DOI:10.1002/ece3.4249
-
2017
- van Meeningen Y., Wang M., Karlsson T., Seifert A., Schurgers G., Rinnan R., and Holst T. (2017): Isoprenoid emission variation of Norway spruce across a European latitudinal transect. Atmospheric Environment, 170:45-57, DOI:10.1016/j.atmosenv.2017.09.045, PDF [1.4MB]
-
2015
- Kadygrov N., Broquet G., Chevallier F., River L., Gerbig C., and Ciais P. (2015): On the potential of the ICOS atmospheric CO2 measurement network for estimating the biogenic CO2 budget of Europe. Atmos. Chem. Phys., 15:12765-12787, DOI:10.5194/acp-15-12765-2015, PDF [6.1MB]
Picture gallery (click on the pictures to enlarge)