@article{Chrysoulakis2018,
title = {Urban energy exchanges monitoring from space},
author = {Nektarios Chrysoulakis and Sue Grimmond and Christian Feigenwinter and Fredrik Lindberg and Jean-Philippe Gastellu-Etchegorry and Mattia Marconcini and Zina Mitraka and Stavros Stagakis and Ben Crawford and Frans Olofson and Lucas Landier and William Morrison and Eberhard Parlow },
editor = {nature.com},
url = {http://urbanfluxes.eu/wp-content/uploads/2018/07/UF_Overview_final.pdf},
doi = {10.1038/s41598-018-29873-x},
issn = {2045-2322},
year = {2018},
date = {2018-07-31},
journal = { nature.com },
volume = {Scientific Reports volume},
number = {8},
pages = {11498},
abstract = {One important challenge facing the urbanization and global environmental change community is to understand the relation between urban form, energy use and carbon emissions. Missing from the current literature are scientific assessments that evaluate the impacts of different urban spatial units on energy fluxes; yet, this type of analysis is needed by urban planners, who recognize that local scale zoning affects energy consumption and local climate. Satellite-based estimation of urban energy fluxes at neighbourhood scale is still a challenge. Here we show the potential of the current satellite missions to retrieve urban energy budget fluxes, supported by meteorological observations and evaluated by direct flux measurements. We found an agreement within 5% between satellite and in-situ derived net all-wave radiation; and identified that wall facet fraction and urban materials type are the most important parameters for estimating heat storage of the urban canopy. The satellite approaches were found to underestimate measured turbulent heat fluxes, with sensible heat flux being most sensitive to surface temperature variation (−64.1, +69.3 W m−2 for ±2 K perturbation). They also underestimate anthropogenic heat fluxes. However, reasonable spatial patterns are obtained for the latter allowing hot-spots to be identified, therefore supporting both urban planning and urban climate modelling.},
keywords = {anthropogenic heat emission, Anthropogenic Heat Flux, Concentration profiles, Copernicus Sentinels, Earth Observation, Eddy-covariance, Flux measurements, Ground-based thermography, Image classification, reducing, Sensor view modelling, Street canyon, Thermographic camera modelling, Understanding, Upwelling longwave radiation, urban, Urban Climate, Urban Energy Budget, urban heat fluxes, Urban meteorology},
pubstate = {published},
tppubtype = {article}
}

@article{Kent2017b,
title = {Aerodynamic roughness parameters in cities: Inclusion of vegetation},
author = {Christoph Kent and Sue Grimmond and David Gatey},
editor = {Journal of Wind Engineering & Industrial Aerodynamics},
url = {http://urbanfluxes.eu/wp-content/uploads/2018/01/2017_Kent_et_al_JWEIA.pdf},
year = {2017},
date = {2017-10-01},
journal = {Journal of Wind Engineering and Industrial Aerodynamics},
volume = {Volume 169},
pages = {168-176},
abstract = {A widely used morphometric method (Macdonald et al. 1998) to calculate the zero-plane displacement (zd) and aerodynamic roughness length (z0) for momentum is further developed to include vegetation. The adaptation also applies to the Kanda et al. (2013) morphometric method which considers roughness-element height variability. Roughness-element heights (mean, maximum and standard deviation) of both buildings and vegetation are combined with a porosity corrected plan area and drag formulation. The method captures the influence of vegetation (in addition to buildings), with the magnitude of the effect depending upon whether buildings or vegetation are dominant and the porosity of vegetation (e.g. leaf-on or leaf-off state). Application to five urban areas demonstrates that where vegetation is taller and has larger surface cover, its inclusion in the morphometric methods can be more important than the morphometric method used. Implications for modelling the logarithmic wind profile (to 100 m) are demonstrated. Where vegetation is taller and occupies a greater amount of space, wind speeds may be slowed by up to a factor of three},
keywords = {Aerodynamic roughness length, Drag coefficient for vegetation, Logarithmic wind profile, Morphometric method, urban, Zero-plane displacement},
pubstate = {published},
tppubtype = {article}
}

@periodical{Feigenwinter2017j,
title = {Insights from more than ten years of CO2 flux measurements in the city of Basel, Switzerland},
author = {Christian Feigenwinter and Michael Schmutz and Roland Vogt and Eberhard Parlow },
editor = {Christian Feigenwinter and Michael Schmutz and Roland Vogt and Eberhard Parlow },
url = {http://urbanfluxes.eu/wp-content/uploads/2018/01/2017_Feigenwinter_et_al_IntAssocUrbClim1.pdf},
year = {2017},
date = {2017-08-01},
issuetitle = {International Association for Urban Climate},
journal = {Urban Climate News, Quarterly Newsletter of the International Association for Urban Climate},
volume = {Issue NO. 65 September 2017},
pages = {24-32},
keywords = {Basel, Carbon-dioxide, Concentration profiles, Eddy-covariance, Flux measurements, Street canyon, urban},
pubstate = {published},
tppubtype = {periodical}
}

@article{Wicki2017bc,
title = {Multiple Regression Analysis for Unmixing of Surface Temperature Data in an Urban Environment},
author = {Andreas Wicki and Eberhard Parlow },
editor = {MDPI},
url = {http://urbanfluxes.eu/wp-content/uploads/2018/01/2017_Wicki_Parlow_RemSens.pdf},
year = {2017},
date = {2017-07-04},
journal = {Remote Sensing},
volume = {Vol 9},
pages = {684},
abstract = {Global climate change and increasing urbanization worldwide intensify the need for a better understanding of human heat stress dynamics in urban systems. During heat waves, which are expected to increase in number and intensity, the development of urban cool islands could be a lifesaver for many elderly and vulnerable people. The use of remote sensing data offers the unique possibility to study these dynamics with spatially distributed large datasets during all seasons of the year and including day and night-time analysis. For the city of Basel 32 high-quality Landsat 8 (L8) scenes are available since 2013, enabling comprehensive statistical analysis. Therefore, land surface temperature (LST) is calculated using L8 thermal infrared (TIR) imagery (stray light corrected) applying improved emissivity and atmospheric corrections. The data are combined with a land use/land cover (LULC) map and evaluated using administrative residential units. The observed dependence of LST on LULC is analyzed using a thermal unmixing approach based on a multiple linear regression (MLR) model, which allows for quantifying the gradual influence of different LULC types on the LST precisely. Seasonal variations due to different solar irradiance and vegetation cover indicate a higher dependence of LST on the LULC during the warmer summer months and an increasing influence of the topography and albedo during the colder seasons. Furthermore, the MLR analysis allows creating predicted LST images, which can be used to fill data gaps like in SLC-off Landsat 7 ETM+ data. Multiple Regression Analysis for Unmixing of Surface Temperature Data in an Urban Environment (PDF Download Available). Available from: https://www.researchgate.net/publication/318206742_Multiple_Regression_Analysis_for_Unmixing_of_Surface_Temperature_Data_in_an_Urban_Environment [accessed Jan 18 2018].},
keywords = {atmospheric corrections, land surface temperature, land use/land cover, Landsat 8, LST analysis, multiple linear regression, thermal infrared data, urban},
pubstate = {published},
tppubtype = {article}
}

@conference{Feigenwinter2017,
title = {Spatial Distribution of Sensible and Latent Heat Flux in the URBANFLUXES case study city Basel (Switzerland)},
author = {Christian Feigenwinter and Eberhard Parlow and Roland Vogt and Michael Schmutz and Nektarios Chrysoulakis and Fredrik Lindberg and Mattia Marconcini and Fabio del-Frate },
editor = {Joint Urban Remote Sensing Event (JURSE)},
url = {http://urbanfluxes.eu/wp-content/uploads/2018/01/2017_Feigenwinter_et_al_JURSE.pdf},
doi = {10.1109/JURSE.2017.7924594},
issn = {978-1-5090-5808-2},
year = {2017},
date = {2017-05-11},
abstract = {Turbulent sensible and latent heat fluxes are calculated by a combined method using micrometeorological approaches (the Aerodynamic Resistance Method ARM), Earth Observation (EO) data and GISTechniques. The spatial distributions of turbulent heat fluxes were analyzed for 22 for the city of Basel (Switzerland), covering all seasons and different meteorological conditions. Seasonal variations in heat fluxes are strongly dependent on meteorological conditions, i.e. air temperature, water vapor saturation deficit and wind speed. The agreement of measured fluxes (by the Eddy Covariance method) with modeled fluxes in the weighted source area of the flux towers is moderate due to known drawbacks in the modelling approach and uncertainties inherent to EC measurements, particularly also in urban areas},
keywords = {Basel, Carbon-dioxide, Concentration profiles, Eddy-covariance, Flux measurements, Street canyon, urban},
pubstate = {published},
tppubtype = {conference}
}

@article{Wicki2017b,
title = {Attribution of local climate zones using a multitemporal land use/land cover classification scheme},
author = {Andreas Wicki and Eberhard Parlow},
editor = {SPIE },
url = {http://urbanfluxes.eu/wp-content/uploads/2018/01/2017_Wicki_Parlow_JARS.pdf},
doi = {DOI: 10.1117/1.JRS.11.026001},
year = {2017},
date = {2017-04-03},
journal = {J. Appl. Remote Sens. 11(2), 026001 (2017)},
volume = {Vol. 11},
pages = {026001-1 – 026001-16},
abstract = {Worldwide, the number of people living in an urban environment exceeds the rural population with increasing tendency. Especially in relation to global climate change, cities play a major role considering the impacts of extreme heat waves on the population. For urban planners, it is important to know which types of urban structures are beneficial for a comfortable urban climate and which actions can be taken to improve urban climate conditions. Therefore, it is essential to differ between not only urban and rural environments, but also between different levels of urban densification. To compare these built-up types within different cities worldwide, Stewart and Oke developed the concept of local climate zones (LCZ) defined by morphological characteristics. The original LCZ scheme often has considerable problems when adapted to European cities with historical city centers, including narrow streets and irregular patterns. In this study, a method to bridge the gap between a classical land use/land cover (LULC) classification and the LCZ scheme is presented. Multitemporal Landsat 8 data are used to create a high accuracy LULC map, which is linked to the LCZ by morphological parameters derived from a high-resolution digital surface model and cadastral data. A bijective combination of the different classification schemes could not be achieved completely due to overlapping threshold values and the spatially homogeneous distribution of morphological parameters, but the attribution of LCZ to the LULC classification was successful. © The Authors. Published by SPIE under a Creative Commons Attribution 3.0 Unported License. Distribution or reproduction of this work in whole or in part requires full attribution of the original publication, including its DOI.},
keywords = {land use/land cover, Landsat 8, local climate zones, morphology, urban},
pubstate = {published},
tppubtype = {article}
}