Award Abstract # 1112938
CAREER: Towards a Better Understanding of Turbulence Structures in a Disturbed Atmospheric Surface Layer

NSF Org: AGS
Division of Atmospheric and Geospace Sciences
Recipient: WASHINGTON STATE UNIVERSITY
Initial Amendment Date: February 25, 2011
Latest Amendment Date: May 27, 2014
Award Number: 1112938
Award Instrument: Standard Grant
Program Manager: edward bensman
AGS
 Division of Atmospheric and Geospace Sciences
GEO
 Directorate for Geosciences
Start Date: August 16, 2010
End Date: April 30, 2016 (Estimated)
Total Intended Award Amount: $425,565.00
Total Awarded Amount to Date: $474,960.00
Funds Obligated to Date: FY 2009 = $425,565.00
FY 2014 = $49,395.00
History of Investigator:
  • Heping Liu (Principal Investigator)
    heping.liu@wsu.edu
Recipient Sponsored Research Office: Washington State University
240 FRENCH ADMINISTRATION BLDG
PULLMAN
WA  US  99164-0001
(509)335-9661
Sponsor Congressional District: 05
Primary Place of Performance: Washington State University
240 FRENCH ADMINISTRATION BLDG
PULLMAN
WA  US  99164-0001
Primary Place of Performance
Congressional District:
05
Unique Entity Identifier (UEI): XRJSGX384TD6
Parent UEI:
NSF Program(s): Physical & Dynamic Meteorology,
EPSCoR Co-Funding
Primary Program Source: 01000910DB NSF RESEARCH & RELATED ACTIVIT
01001415DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 0000, 1045, 1525, 4444, 9150, OTHR
Program Element Code(s): 152500, 915000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

The Monin-Obukhov similarity theory (MOST) provides numerical weather and climate models with a basis in formulating the turbulent exchange of momentum, energy, water vapor, and other scalars between the Earth's surface and the lower atmosphere. However, several recent studies have identified some features that are not fully consistent with predictions by MOST and attributed these departures to the disturbance of outer-layer, large-scale coherent structures (hereafter referred to as coherent eddies) on locally-generated active turbulence in the atmospheric surface layer (ASL). Although some studies have presented alternative theories to describe these discrepancies, turbulence structures in the disturbed ASL are still poorly understood. The objectives of this project are to study turbulence structures in the stable and unstable ASL beneath a convective boundary layer where a strong interaction between coherent eddies and active turbulence occurs. The datasets from the already completed Energy Balance Experiment will be used. More specifically, this project aims to:

1. Quantify turbulence structures under the influence of large-scale coherent eddies and characterize the deviations of turbulence structures from predictions by MOST under two atmospheric stratifications during the daytime in the disturbed ASL.

2. Investigate how coherent eddies interact with the ASL turbulence and their contributions to flux exchange of momentum, heat, and water vapor under two atmospheric stratifications.

3. Study the spatial structures and temporal evolutions of coherent eddies from time-series data in the ASL to elucidate the origins and sources of coherent eddies.

4. Enhance the Jackson State University Micrometeorology Laboratory and enrich meteorological courses through incorporating research activities and findings of this project in the classroom and teaching laboratories.

5. Involve a large number of African American undergraduate and graduate students and encourage them to take part in the research activities.

This program will provide an excellent education and training opportunity for undergraduate and graduate students and will greatly enhance atmospheric sciences education in Jackson State University, one of the nation's largest historically black colleges and universities.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Qianyu Zang and Heping Liu "Interannual variability in the surface energy budget and evaporation over a large southern inland water in the United States" Journal of Geophysical Research - Atmospheres , v.118 , 2013 , p.13 doi:10.1002/jgrd.50435

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

In numerical weather and climate models, turbulent transfer of heat, water vapor, and other greenhouse gases in the atmospheric surface layer (ASL) is formulated using the so-called Monin-Obukhov similarity theory (MOST). The MOST assumes that flows in the stationary ASL depend on only local mechanical mixing and thermodynamic processes. Since the MOST is framed in terms of local parameters and is only applied for locally-generated, active turbulence, therefore, it implies that the non-locally generated atmospheric motions in the atmospheric boundary layer (ABL) have no significant effects on flows in the ASL. However, studies have identified some features not fully consistent with the MOST, attributed largely to the influence of non-local, large coherent eddies on the locally-generated active turbulence in the ASL. The research supported by this award was designed to study how large coherent eddies disturb the ASL, thus affecting turbulence structures, flux exchange, and unclosure of the surface energy balance in the ASL. The results of our study gave us a number of new insights into the interactions between large coherent eddies and the ASL, small-scale turbulence. Specifically, our results indicate that spatial scales of large coherent eddies are related to those of soil moisture heterogeneity; large coherent eddies modulate time-series of vertical velocity and scalars (e.g., air temperature and humidity) in different ways leading to temporal variations in fluxes; the increased phase shifts between vertical velocity and scalars of large eddies, leading to the decreased fluxes and thus an increase in unclosure in the surface energy balance.

Six undergraduate students including five African-American students and one Latino student participated in the research in this project; two master students were supported by this project and graduated; Two Ph.D. students have been supported by this project: one graduated in July 2015 and the other is expected to graduate in July 2017. Eleven peer-reviewed journal articles were published, three manuscripts are in preparation and will be submitted to peer-reviewed journals in the next few months, and seventeen conference presentations were made to disseminate our research outcomes to broad communities. Our research results were reported in public media and also cited in the Top Story of the NSF Science360 News. The two courses taught by the PI incorporated the findings of this project in the syllabi, lectures, and field experiments for both undergraduate and graduate education. 


Last Modified: 08/01/2016
Modified by: Heping Liu

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