Tim Logan

 Tim Logan

Tim Logan

  • Courses2
  • Reviews9

Biography

Texas A&M University College Station - Life Science


Resume

  • 2009

    Doctor of Philosophy (Ph.D.)

    Atmospheric Sciences and Meteorology

    The University of North Dakota

  • 2007

    M.S.

    Atmospheric Science

    AGU

    Intramural Hockey and Broomball

    Grand Forks Curling Club

    The University of North Dakota

  • 1989

    BA

    Environmental Science

    University of Virginia

  • Dr. Tim Logan

    I AM STUDYING THE PHYSICO-CHEMICAL PROPERTIES OF AEROSOLS BASED ON THEIR ABSORPTION OF LIGHT RANGING FROM THE SHORTWAVE TO INFRARED WAVELENGTHS USING GROUND BASED AERONET AND SATELLITE DATA.

    Scientific Computing

    Geology

    Meteorology

    IDL

    LaTeX

    Earth Science

    Science

    Physics

    Mathematica

    Oceanography

    Fortran

    Mathematical Modeling

    Astronomy

    Weather Forecasting

    A study of Asian dust plumes using satellite

    surface

    and aircraft measurements during the INTEX-B field experiment

    Maureen Cribb

    Zhanqing Li

    Xiquan Dong

    Baike Xi

    Study based on Asian dust and pollution transport from the combined masters theses of Appleford and Logan.

    A study of Asian dust plumes using satellite

    surface

    and aircraft measurements during the INTEX-B field experiment

    Jilin Sun

    Wenjun Qu

    Xu Dong

    Lifang Sheng

    Wencai Wang

    Journal of Quantitative Spectroscopy & Radiative Transfer

    Dust aerosol effect on the retrievals of dusty cloud top height (DCTH) are analyzed over Northwest China using cloud products from MODerate Resolution Imaging Spectroradiometer (MODIS) on Aqua

    Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO)

    and CloudSat for the Spring season of March–May over the years 2007–2011. An excellent agreement is found between CloudSat and CALIPSO derived DCTHs for all cloud types

    suggesting that the effect of dust aerosols plays a small role in DCTHs determination for lidar and radar measurements. However

    the presence of dust aerosols greatly affects the retrievals of DCTHs for MODIS compared with pure clouds and the active sensors derived results. The differences of DCTHs retrieving from CloudSat and MODIS range from −2.30 to 6.8 km. Likewise

    the differences of DCTHs retrieving from CALIPSO and MODIS range from −2.66 to 6.78 km. In addition

    the results show that the differences in DCTHs for active and passive sensors are dependent on cloud type. On the whole

    dust aerosols have the largest effect on cloud top heights (CTH) retrieved of nimbostratus (Ns)

    followed by altocumulus (Ac) and altostratus (As)

    the last is cirrus (Ci) over Northwest China. Our results also indicate that the accuracy of MODIS-derived retrievals reduces accompanied with a decrease of height.

    Dust aerosol impact on the retrieval of cloud top height from satellite observations of CALIPSO

    CloudSat and MODIS

    Lead author is Ron Li

    Co-authors: G. Tang

    J. Ding. T. Logan

    S. Brooks

    D. R. Collins

    P. Yang

    and G. W. Kattawar\nRetrieval of aerosol scattering properties using laser spectroscopy apparatus developed by Dr. Ping Yang and his research scientist Ron Li.

    Laboratory measurements of light scattering properties of kaolinite dust at 532 nm

    Xiquan Dong

    Baike Xi

    Biomass burning aerosols can have a large impact on atmospheric processes as well as human health. During the 2012 warm season

    a large outbreak of wildfires originating from the intermountain and Pacific states provided many opportunities to observe the physical and chemical properties of biomass smoke aerosols. Six biomass burning smoke plumes (26 June – 15 September) have been observed by the newly installed Grand Forks

    North Dakota

    AERONET site (47.91ºN

    97.32ºW) and are selected for this study. To identify the source regions

    HYSPLIT backward trajectory model data and satellite imagery are used to track these events. The volume size distribution and spectral aerosol optical depth (AOD) dependence showed the relative influences of fine and coarse mode particles. Case II (4 July) had the strongest fine mode influence as evidenced by a strong spectral AOD dependence while Case VI (15 September) had the strongest coarse mode influence with the weakest spectral dependence. The spectral dependences of absorption aerosol optical depth (AAOD) and single scattering co-albedo (oabs) illustrated the varying absorption of the smoke plumes by inferring the relative contributions of strongly and weakly absorbing carbonaceous species. More specifically

    the AAOD parameter is primarily influenced by aerosol particle size while oabs is more dependent on aerosol composition. The AAOD spectral dependences for Cases I (26 June)

    III (31 July)

    and VI were weaker than those from Cases II

    IV (28 August)

    and V (30 August). However

    the spectral oabs dependences were different in that the smoke particles in Cases III and VI had the strongest absorption while Cases I

    II

    IV

    and V had moderate to weakly absorbing particles. In addition

    a weak correlation was found between plume transport time and particle absorption where strongly absorbing carbon was converted to weakly absorbing carbon.

    Biomass Burning Aerosol Properties over the Northern Great Plains during the 2012 Warm Season

    Maureen Cribb

    Zhanqing Li

    Xiquan Dong

    Baike Xi

    Aerosol classification method based on the absorptive properties of aerosols. Aerosol organic chemistry can also be inferred.

    Classification and investigation of Asian aerosol absorptive properties

    Wei Gong

    Feiyue Mao

    Optics Express

    The automatic detection of aerosols and the cloud layer boundary (base and top) is important in atmospheric lidar data processing

    because the boundary information is not only useful for environment and climate studies

    but can also be used as input for further data processing. Previous methods have demonstrated limitations in defining the base and top

    window-size setting

    and have neglected the in-layer attenuation. To overcome these limitations

    we present a new layer detection scheme based on linear segmentation with a reasonable threshold setting

    boundary selecting

    and over-detection removing strategies. Preliminary results from both real and simulated data show that this algorithm can not only detect the layer-base as accurate as the simple multi-scale method

    but also can detect layer-top more accurately than that of the simple multi-scale method. Our algorithm can be directly applied to uncalibrated data without requiring any additional measurements or window size selections.

    Detecting layer in atmospheric lidar signal based on linear segmentation

    Impacts of biomass burning smoke on deep convection and lightning polarity.

    Anomalous Lightning Behavior during the 26-27 August 2007 Northern Great Plains Severe Weather Event

    Impacts of biomass burning smoke aerosols on low-level cloud development. Co-authors: Dr. Xiquan Dong and Dr. Baike Xi

    Aerosol properties and their impacts on surface CCN at the ARM Southern Great Plains site during the 2011 Midlatitude Continental Convective Clouds Experiment

    Xiquan Dong

    Baike Xi

    Comparison of two strong winter and spring season dust events over three Asian sites representing urban/pollution

    mineral dust

    and mixed type aerosol generation regions.

    A comparison of the mineral dust absorptive properties between two Asian dust events

    Xiquan Dong

    Baike Xi

    A multiplatform data set from the Clouds

    Aerosol

    and Precipitation in the Marine Boundary Layer (MBL) Graciosa

    Azores

    2009–2010 field campaign was used to investigate how continental aerosols can influence MBL cloud condensation nuclei (CCN) number concentration (NCCN). The seasonal variations of aerosol properties have shown that the winter and early spring months had the highest mean surface wind speed (> 5 m s−1) and greatest contribution of sea salt to aerosol optical depth (AOD)

    while continental fine mode aerosols were the main contributors to AOD during the warm season months (May–September). Five aerosol events consisting of mineral dust

    pollution

    biomass smoke

    and volcanic ash particles were selected as case studies using Atmospheric Radiation Measurement (ARM) mobile facility measurements. The aerosols in Case I were found to primarily consist of coarse mode

    Saharan mineral dust. For Case II

    the aerosols were also coarse mode but consisted of volcanic ash. Case III had fine mode biomass smoke and pollution aerosol influences while Cases IV and V consisted of mixtures of North American pollution and Saharan dust that was advected by an extratropical cyclone to the Azores. Cases I

    IV

    and V exhibited weak correlations between aerosol loading and NCCN due to mineral dust influences

    while Cases II and III had a strong relationship with NCCN likely due to the sulfate content in the volcanic ash and pollution particles. The permanent Eastern North Atlantic ARM facility over the Azores will aid in a future long-term study of aerosol effects on NCCN.

    Aerosol properties and their influences on marine boundary layer cloud condensation nuclei at the ARM mobile facility over the Azores

    Director of the Houston Lightning Mapping Array (HLMA) Network. The HLMA provides a service to the surrounding community by providing timely and reliable lightning data to make informed decisions in regards to public safety interests while providing quality data for collaborative

    interdisciplinary research within the university community and for K-12 STEM projects. As part of this effort

    I develop and test sferics detectors under various modes of deep convection.\n\nMy current research deals with aerosol impacts on low-level cloud development which is funded by a NSF Grant (2017-2020). As part of the grant

    I develop micro-gadgets capable of measuring temperature

    pressure

    and aerosol optical depth. As part of the Texas A&M University Tier One Proposal (TOPS) grant (2018-2021)

    I study aerosol impacts on boundary layer clouds using 3-D images derived from a portable micropulse LIDAR.\n\nMy primary research goals are to (1) improve upon earlier aerosol classification methods by using theoretical radiative transfer calculations and in situ measurements (e.g.

    laser spectroscopy)

    (2) analyze the long-term aerosol impacts on low-level and deep convective cloud development

    and (3) discern the possible impacts of biomass burning smoke aerosols on severe weather and lightning.\n\n\nSpecialties: Fluent in Spanish

    semi-fluent in French and German

    great public speaking skills

    proficient in IDL computing language

    Tim

    Logan

    Texas A&M University

    Morristown High School

    University of North Dakota

    Develop and implement lessons for topics dealing with the basic mechanics of the atmosphere and relating these topics to undergraduate students who are non-atmospheric science majors.

    Instructional Assistant Professor

    Bryan/College Station

    Texas Area

    Texas A&M University

    Morristown

    New Jersey

    Create and implement a curriculum based upon the four core areas of earth science systems (geology

    oceanography

    meteorology

    and astronomy) in addition to selected topics in modern and classical physics. This curriculum is also infused with hands-on learning based technology developed by PITSCO.

    Geophysical Systems Science Teacher

    Morristown High School

    Develop an aerosol classification method in order to interpret the effects of various aerosol types on the Earth's radiation budget

    cloud microphysical properties and deep convective processes.

    Graduate Research Assistant

    Grand Forks

    North Dakota Area

    University of North Dakota

    Summary of published study that investigates the influences of several types of aerosols on marine boundary layer (MBL) cloud condensation nuclei (CCN).

    American Meteorological Society

ATMO 201

4.4(8)