Atmosphere–Biosphere Interaction Monitoring and Modelling: Impact on Meteorological and Climate Conditions at Small Scales

A special issue of Atmosphere (ISSN 2073-4433). This special issue belongs to the section "Biosphere/Hydrosphere/Land–Atmosphere Interactions".

Deadline for manuscript submissions: closed (1 July 2021) | Viewed by 5066

Special Issue Editors


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Guest Editor
University of Novi Sad, Novi Sad, Serbia
Interests: biosphere–atmosphere interaction; dynamical modeling; efficacy of weather forecast application; agrometeorology
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E-Mail Website
Guest Editor
Institute of Meteorology and Climatology, University of Natural Resources and Life Sciences, Gregor-Mendel-Straße 33, 1180 Wien, Austria
Interests: agricultural meteorology; agroclimatology; microclimatology; remote sensing in agricultural meteorology; simulation models (agro-ecosystems, crops)
Special Issues, Collections and Topics in MDPI journals

Special Issue Information

Dear Colleagues,

We invite you to contribute original research articles, as well as review articles, dealing with all aspects of biosphere–atmosphere interaction measurement and modeling and its impact on weather and climate at small scales. Expected contributions include recent experimental and modeling works, techniques, and developments tailored to the assessment of the most important processes related to biosphere–atmosphere interaction and their effects in rural and urban microenvironments. In this Special Issue, particular attention will be devoted to micrometeorological measurements. Therefore, descriptions and reviews of long-term micrometeorological measurements in rural (including forests) and urban environments are welcome. We are also interested in reviews with possible future lines of research topics. Topics of interest include but are not limited to:

  • Seasonality of micrometeorological conditions;
  • parameterization of processes describing biosphere–atmosphere interaction;
  • Micrometeorological and biological observations;
  • Impact of biometeorological conditions on plant disease and harmful organism development;
  • Impact of plants/vegetation on urban microclimate;
  • Extreme temperature variation in presence of vegetation;
  • Micrometeorological measurements in rural and urban areas.

Prof. Dr. Branislava Lalić
Prof. Dr. Josef Eitzinger
Guest Editors

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Keywords

  • Biosphere–atmosphere interaction
  • Micrometeorological and biological observations
  • Weather and climate sensitivity to biosphere-atmosphere exchange
  • Agro- and forest micrometeorology
  • Urban micrometeorology

Published Papers (2 papers)

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Research

22 pages, 4270 KiB  
Article
Maximum, Minimum, and Daily Air Temperature Range in Orchards: What Do Observations Reveal?
by Ana Firanj Sremac, Branislava Lalic, Joan Cuxart and Milena Marcic
Atmosphere 2021, 12(10), 1279; https://0-doi-org.brum.beds.ac.uk/10.3390/atmos12101279 - 30 Sep 2021
Cited by 5 | Viewed by 1670
Abstract
This study was designed to better understand vegetation’s impact on air maximum (Tmax), minimum (Tmin), and daily temperature range (DTR), as well as seasonality and variability. We selected a flat, under synoptic-scale, northern Serbian region with an operational network [...] Read more.
This study was designed to better understand vegetation’s impact on air maximum (Tmax), minimum (Tmin), and daily temperature range (DTR), as well as seasonality and variability. We selected a flat, under synoptic-scale, northern Serbian region with an operational network of automated weather stations (AWS) for the study. Data were collected directly from the eighteen AWSs placed in the orchard canopy during 2013–2018. Meteorological data, plant phenological data in the form of the BBCH scale, and orchards’ soil characteristics data were collected. Environmental factors influencing the temperature were classified as static (slow or unchangeable) and dynamic (fast-changing). The impact of both factors on maximum, minimum, and daily temperature range and its variability were analyzed. Results show that static factors (like soil texture) affect the annual variation of Tmax, Tmin, and DTR rather than its variability over the season. The dynamic factors, mainly coming from the plant’s phenology, substantially affected the seasonal variability of these variables. Studies like this suffer from missing data and sparse spatial coverage by the AWS network. Therefore, the alternatives of orchard micrometeorological data, nearest climatological station, and ERA5-Land reanalysis data are tested. Both data sets showcased limitations in their applicability, while reanalysis data deviated more from the in-situ measurements, both seasonally and regionally. Full article
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36 pages, 10718 KiB  
Article
Simulation of Daily Mean Soil Temperatures for Agricultural Land Use Considering Limited Input Data
by Philipp Grabenweger, Branislava Lalic, Miroslav Trnka, Jan Balek, Erwin Murer, Carmen Krammer, Martin Možný, Anne Gobin, Levent Şaylan and Josef Eitzinger
Atmosphere 2021, 12(4), 441; https://0-doi-org.brum.beds.ac.uk/10.3390/atmos12040441 - 29 Mar 2021
Cited by 2 | Viewed by 2789
Abstract
A one-dimensional simulation model that simulates daily mean soil temperature on a daily time-step basis, named AGRISOTES (AGRIcultural SOil TEmperature Simulation), is described. It considers ground coverage by biomass or a snow layer and accounts for the freeze/thaw effect of soil water. The [...] Read more.
A one-dimensional simulation model that simulates daily mean soil temperature on a daily time-step basis, named AGRISOTES (AGRIcultural SOil TEmperature Simulation), is described. It considers ground coverage by biomass or a snow layer and accounts for the freeze/thaw effect of soil water. The model is designed for use on agricultural land with limited (and mostly easily available) input data, for estimating soil temperature spatial patterns, for single sites (as a stand-alone version), or in context with agrometeorological and agronomic models. The calibration and validation of the model are carried out on measured soil temperatures in experimental fields and other measurement sites with various climates, agricultural land uses and soil conditions in Europe. The model validation shows good results, but they are determined strongly by the quality and representativeness of the measured or estimated input parameters to which the model is most sensitive, particularly soil cover dynamics (biomass and snow cover), soil pore volume, soil texture and water content over the soil column. Full article
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