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Research Interests

Philosophy and Approach: I am interested in how components of the earth system interact, emphasizing investigation between land, atmosphere, and atmospheric chemistry. Below are particular topics and questions that I find most exciting.  I like attacking these questions by really digging into the process-level mechanisms responsible for producing observed relationships starting from first principles.  My ...

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Research Interests | ahmedbtawfik.com Reviews
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Philosophy and Approach: I am interested in how components of the earth system interact, emphasizing investigation between land, atmosphere, and atmospheric chemistry. Below are particular topics and questions that I find most exciting.  I like attacking these questions by really digging into the process-level mechanisms responsible for producing observed relationships starting from first principles.  My ...
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2 about me
3 publications
4 research
5 research interests
6 code
7 tech skills
8 latest news
9 ideas out loud
10 philosophy and approach
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Research Interests | ahmedbtawfik.com Reviews

https://ahmedbtawfik.com

Philosophy and Approach: I am interested in how components of the earth system interact, emphasizing investigation between land, atmosphere, and atmospheric chemistry. Below are particular topics and questions that I find most exciting.  I like attacking these questions by really digging into the process-level mechanisms responsible for producing observed relationships starting from first principles.  My ...

INTERNAL PAGES

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1

Publications

http://www.ahmedbtawfik.com/publications

8212;—Atmospheric Science, Research Scientist——. Tawfik, A.,. PA Dirmeyer, J.A. Santanello Jr. (2015), The Heated Condensation Framework. Part I: Description and Southern Great Plains Case Study, Journal of Hydromet. Doi: 10.1175/JHM-D-14-0117.1. Tawfik, A.,. PA Dirmeyer, J.A. Santanello Jr. (2015), The Heated Condensation Framework. Part II: Climatological behavior of convective initiation and land-atmosphere coupling over the Continental United States, Journal of Hydromet. Tawfik, A.B.,. Ouimette, A&#4...

2

Ideas Out Loud

http://www.ahmedbtawfik.com/thinking-out-loud

8212;—Atmospheric Science, Research Scientist——. Convective Parameterizations: Fuzzy Terminology. The treatment of clouds in general circulation models was always a bit of a puzzle to me. I remember thinking way back in undergrad “why on Earth would we treat fair weather cumulus, stratiform clouds, and towering cumulus any differently in models? Aren’t they all just RH = 100 % means condensation? Does Surface Energy Partitioning Make Sense? Moist Convection: initiation versus intensity feedbacks.

3

Code

http://www.ahmedbtawfik.com/code

8212;—Atmospheric Science, Research Scientist——. Buoyant Condensation Level -. Defines the height the boundary layer needs to reach in order for saturation to occur. When Can It Be Calculated:. Calculable for any atmospheric profile with sufficient resolution to capture moisture and temperature structure. Most suitable for atmospheric soundings and model output with more than 20 vertical levels in the troposphere. Potential Temperature Deficit -. Defines the surface temperature increase necessary to reac...

4

About Me

http://www.ahmedbtawfik.com/about-me

8212;—Atmospheric Science, Research Scientist——. National Center for Atmospheric Research. Climate and Global Dynamics. Project Scientist I (. Center for Ocean-Land-Atmosphere Studies. Earth System Modeling Postdoctoral Fellow. Department of Atmospheric, Oceanic, and Space Sciences. PhD in Atmo. Sci. 2012. MS in Atmo. Sci. 2008. North Carolina State University. Department of Marine, Earth, & Atmospheric Sciences. BS in Meteorology 2007. BS in Marine Sci. 2007.

5

Technical Skills

http://www.ahmedbtawfik.com/technical-skills

8212;—Atmospheric Science, Research Scientist——. NCAR Common Language (NCL). Python – matplotlib. Climate Data Operators (cdo).

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Convective Triggering Potential | Coupling Metrics

http://www.coupling-metrics.com/convective-triggering-potential

How to Use it. Using morning vertical profiles (e.g. atmospheric soundings), the convective triggering potential and low-level dew point depression (. Identify whether convection is more likely to be initiated over dry versus wet soils. Quantifies how primed the atmosphere is to moist convection. The. Measures the stability, and. When constrained by observations or model estimates, the. When evaporative fraction available and. Being on the x-axis and. Surface sensible heat flux. Distinctions between wet ...

coupling-metrics.com coupling-metrics.com

Soil Moisture Memory | Coupling Metrics

http://www.coupling-metrics.com/soil-moisture-memory

How to Use it. Assesses the ability of soil to retain its moisture state, or more specifically the time it takes for soil moisture to decay to a condition beyond 1/e. Quantifies the time it takes for soil moisture to lose information of its initial state, meaning the time it takes for the lagged autocorrelation of soil moisture to fall below its e. Be cautious when comparing soil moisture memory across different sites when using in-situ data because measurements may have been taken at various depths or w...

coupling-metrics.com coupling-metrics.com

Heated Condensation Framework | Coupling Metrics

http://www.coupling-metrics.com/heated-condensation

How to Use it. Assesses the atmospheric background state with respect to convective initiation using. Convection can also be identified as having been triggered due to local surface forcing when. Equals zero. Additionally the amount of surface sensible heat flux necessary for triggering convection assuming no additional moisture inputs is defined by. Representing the strictly heat pathway. Conversely the moisture pathway for triggering is quantified by. And Figures 5-8 from Part II. Translate to drier, m...

coupling-metrics.com coupling-metrics.com

Mixing Diagrams | Coupling Metrics

http://www.coupling-metrics.com/mixing-diagrams

How to Use it. Quantifies the heat and moisture entrainment fluxes at the top of the boundary layer, values that are incredibly difficult to quantify. And Santanello et al. (2015). Surface latent heat flux. Surface sensible heat flux. Boundary layer height during the day. For more precise calculations that include horizontal advection, wind speed (. Dim2 , ntim, steps per day , &. T2m , psfc , q2m , &. Pbl h , shf , lhf , dt , &. Shf ent , lhf ent , shf sfc, &. Lhf sfc , shf tot , lhf tot, &. Use the tem...

coupling-metrics.com coupling-metrics.com

Terrestrial Coupling Index | Coupling Metrics

http://www.coupling-metrics.com/terrestrial-coupling-index

How to Use it. Determines the magnitude of coupling between soil moisture and surface fluxes using statistical techniques. Specifically, the terrestrial coupling index uses the daily slope of the soil moisture-surface flux relationship as weighted by the standard deviation in soil moisture to determine the degree to which soil moisture changes drive surface flux variability. But does not require multiple carefully constructed simulations (See Figure 1 from Dirmeyer 2011. And Figure 1 from Part 2. Needs s...

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Research Interests

8212;—Atmospheric Science, Post Doctoral Fellow——. Although there have been tremendous strides in understanding how convection is triggered,. Tawfik, A.,. PA Dirmeyer, J.A. Santanello Jr., The Heated Condensation Framework. Part I: Description and Southern Great Plains Case Study, Journal of Hydromet. Tawfik, A.,. Tawfik, A.B.,. And PA. Dirmeyer (2014), A process-based framework for quantifying the atmospheric preconditioning of surface-triggered convection, Geophys. Res. Lett.,. Or suppressing developme...

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