This document summarizes the development of a model to predict hourly precipitation. It discusses variable selection using correlation analysis, time-lagged correlations between stations, and simulation results to determine the best combination of variables. The model was trained on data from 2011-2013 and tested on random sample data from the same period. Output is a probability prediction for precipitation in each of the next 4 hours. Example output graphs show the model accurately capturing periods of low and average rainfall.
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Disclaimer:
The Royal Irish Academy has prepared the content of this website responsibly and carefully, but disclaims all warranties, express or implied, as to the accuracy of the information contained in any of the materials. The views expressed are the authors’ own and not those of the Royal Irish Academy.
Hydroclimatology of Sariz Creek Watershed, Located In Seyhan Basin, And Simulation Of The Snowmelt Runoff Using Remote Sensing And Geographic Information Systems (Mountain Watershed Case Study). Presented by Ibrahim Gürer at the "Perth II: Global Change and the World's Mountains" conference in Perth, Scotland in September 2010.
Weather!: Meteorology and Meteorological Collections at the Royal Irish Acade...The Royal Irish Academy
Weather!: Meteorology and Meteorological Collections at the Royal Irish Academy and Met Éireann - Mairéad Treanor, Librarian, Met Éireann. For additional information including audio recordings to accompany this presentation please click here - http://www.ria.ie/library/exhibitions/lunchtime-lecture-series.aspx.
Disclaimer:
The Royal Irish Academy has prepared the content of this website responsibly and carefully, but disclaims all warranties, express or implied, as to the accuracy of the information contained in any of the materials. The views expressed are the authors’ own and not those of the Royal Irish Academy.
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This paper applies inverse transform sampling to sample training points for surrogate models. Inverse transform sampling uniformly generates a sequence of real numbers ranging from 0 to 1 as the probabilities at sample points. The coordinates of the sample points are evaluated using the inverse functions of Cumulative Distribution Functions (CDF). The inputs to surrogate models are assumed to be independent random variables. The sample points obtained by inverse transform sampling can effectively represent the frequency of occurrence of the inputs. The distributions of inputs to the surrogate models are fitted to their observed data. These distributions are used for inverse transform sampling. The sample points have larger densities in the regions where the Probability Density Functions (PDF) are higher. This sampling approach ensures that the regions with higher densities of sample points are more prevalent in the observations of the random variables. Inverse transform sampling is applied to the development of surrogate models for window performance evaluation. The distributions of the following three climatic conditions are fitted: (i) the outside temperature, (ii) the wind speed, and (iii) the solar radiation. The sample climatic conditions obtained by the inverse transform sampling are used as training points to evaluate the heat transfer through a generic triple pane window. Using the simulation results at the sample points, surrogate models are developed to represent the heat transfer through the window as a function of the climatic conditions. It is observed that surrogate models developed using the inverse transform sampling can provide higher accuracy than that developed using the Sobol sequence directly for the window performance evaluation.
Remote sensing products in support of crop subsidy in MexicoCIMMYT
Remote sensing –Beyond images
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The workshop was organized by CIMMYT Global Conservation Agriculture Program (GCAP) and funded by the Bill & Melinda Gates Foundation (BMGF), the Mexican Secretariat of Agriculture, Livestock, Rural Development, Fisheries and Food (SAGARPA), the International Maize and Wheat Improvement Center (CIMMYT), CGIAR Research Program on Maize, the Cereal System Initiative for South Asia (CSISA) and the Sustainable Modernization of the Traditional Agriculture (MasAgro)
I encourage you to visit my blog (danherr.com/2012/01/22/ams-renewable-energy-jobs/) for the true transcript of my presentation and the recorded video.
Talk given by Daniel Herr on Job Opportunities for Meteorological Students in Clean Energy at the 2012 American Meteorological Society Conference in New Orleans, Louisiana on Saturday the 21st of January, 2012. **Please be aware that some of the fonts changed the look of the slides during upload**
This presentation created and addressed by Jesús Fernandez (University of Cantabria) in the intensive three day course from the BC3, Basque Centre for Climate Change and UPV/EHU (University of the Basque Country) on Climate Change in the Uda Ikastaroak Framework.
The objective of the BC3 Summer School is to offer an updated and multidisciplinary view of the ongoing trends in climate change research. The BC3 Summer School is organized in collaboration with the University of the Basque Country and is a high quality and excellent summer course gathering leading experts in the field and students from top universities and research centres worldwide.
Factors affecting monsoon precipitation in NepalSagar Parajuli
I did a brief study about the factors affecting monsoon precipitation in Nepal few months ago for a class project. I am sharing the slides as it is relevant to the recent flooding in north India and Nepal.
This paper applies inverse transform sampling to sample training points for surrogate models. Inverse transform sampling uniformly generates a sequence of real numbers ranging from 0 to 1 as the probabilities at sample points. The coordinates of the sample points are evaluated using the inverse functions of Cumulative Distribution Functions (CDF). The inputs to surrogate models are assumed to be independent random variables. The sample points obtained by inverse transform sampling can effectively represent the frequency of occurrence of the inputs. The distributions of inputs to the surrogate models are fitted to their observed data. These distributions are used for inverse transform sampling. The sample points have larger densities in the regions where the Probability Density Functions (PDF) are higher. This sampling approach ensures that the regions with higher densities of sample points are more prevalent in the observations of the random variables. Inverse transform sampling is applied to the development of surrogate models for window performance evaluation. The distributions of the following three climatic conditions are fitted: (i) the outside temperature, (ii) the wind speed, and (iii) the solar radiation. The sample climatic conditions obtained by the inverse transform sampling are used as training points to evaluate the heat transfer through a generic triple pane window. Using the simulation results at the sample points, surrogate models are developed to represent the heat transfer through the window as a function of the climatic conditions. It is observed that surrogate models developed using the inverse transform sampling can provide higher accuracy than that developed using the Sobol sequence directly for the window performance evaluation.
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Come get refreshed on the impact some basic choices in statistical behavior can have on what gets triggered. Learn why a median might be the choice for historical anomaly or sudden change. Jump into Gaussian distributions, data alignment challenges and the trouble with sampling. Walk out with a deeper understanding of your metrics and what they might be telling you.
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Quick, what’s the difference between the mean, the mode and the median? Do you need a Gaussian or a normal distribution And does your choice impact the alerts and observations you get from your observability tools?
Come get refreshed on the impact some basic choices in statistical behavior can have on what gets triggered. Learn why a median might be the choice for historical anomaly or sudden change. Jump into Gaussian distributions, data alignment challenges, and the trouble with sampling. Walk out with a deeper understanding of your metrics and what they might tell you.
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2. Agenda
• Model
• Variable Selection
• Correlation
• Time Lagged Correlations
• Simulation Result
• Variable selection Vs Mean Error
• Input -Neighbor Stations Selections
• Stations which can be used as good predictors
• Cross Correlation Between Stations for Hourly Precipitation
• Correlation Plots
• Results
• Error Plot
• Hourly System output
3. Model
Data Collection Train Network Predict Data Web Interface
Train
Network
Normalize Data.
.
Neural Network Training Section Cubic Spline Interpolation Multiple Sections
Online Prediction and Web Section Trained Neural Network Aggregate Data
4. Variable Selection-Correlation
• Output
• 4 hours of Probability data for
Hourly Precipitation
http://10.39.8.247/predict/correlation.php#div-1
All Variables
Temperature
Humidity
Dew point
Pressure
Wind Speed
Wind Speed Gust
Wind Direction
Wind Direction Degree
Daily Rain
Hourly Precipitation
Selected Variables
Hourly Precipitation
Humidity
Wind Direction
Daily Rain
Solar Radiation
Temperature
5. Cross Correlation Between Variables
HP Vs Humidity HP Vs Pressure HP Vs Solar Radiation
HP Vs Temperature HP Vs Wind Direction Degree HP Vs Wind Speed
*HP- Hourly Precipitation
6. Variable Selection-Cross Correlation
HP Vs Humidity HP Vs Pressure HP Vs Solar Radiation
HP Vs Temperature HP Vs Wind Direction Degree HP Vs Wind Speed
Selected Variables
Hourly Precipitation
Humidity
Wind Direction
Daily Rain
Solar Radiation
Temperature
All Variables
Temperature
Humidity
Dew point
Pressure
Wind Speed
Wind Speed Gust
Wind Direction
Wind Direction Degree
Daily Rain
Hourly Precipitation
Selected Variables
Hourly Precipitation
Humidity
Daily Rain
Wind Direction
Correlation
Cross Correlation
9. Number of Hours of input data
0
0.02
0.04
0.06
0.08
0.1
0.12
0.14
0.16
0 5 10 15 20 25 30
MAE
Number of hours
Number of Input hours of data required
1
1.1
1.2
1.3
1.4
1.5
1.6
1.7
1.8
1.9
0 5 10 15 20 25 30 35
MAE
Number of Neurons
Number of Neurons
• Number of Hours input data- 24
• Number of hidden Neurons=7
10. Stations which can be used as good predictors
0
5
10
15
20
25
-18 -17 -16 -14 -13 -12 -11 -10 -9 -8 -7 -6 -5 -4 -3 -2 -1
COUNT
NUMBER HOURS AHEAD
Number of Times Rainfall occured at stations before IBSURRE21
Burna10
CWWK
Ibccoqui5
Ibcpittm3
Surre10
Surre6
17. Input/output Representation
• Input is 24 hour Normalized data from three stations and 3 variables
from the stations.
• Output is 4 variable. Each variable indicating probability of rain for
every hour ahead.
Date Time Hour1 Hour2 Hour3 Hour4
… 0 0 0 0
…. 0 1 0 0
… 1 0 0 0
…. 0 0 0 1
• Sample Actual OutputData Used for Training
• Rainfall>1(mm) ? Output=1 : Output =0
We Have 2^4= 16 different
Combinations of possible Output
Distribution of Actual Output Classes
2011-2013
18. Error Plot
Predicted
Error Computed for Random Sample data 2011-2013
*This data was not used for Training
Value 0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15
Output Class 0000 0001 0010 0011 0100 0101 0110 0111 1000 1001 1010 1011 1100 1101 1110 1111
Predicted
actual actual
counts percentage
30. Hourly Precipitation Vs Wind Direction
Back time lagged correlation
0
50
100
150
200
250
300
350
Degree
Direction Vs Degress
2013- 6 Hours Prior to Rainfall- Wind Direction Distribution
31. Correlation Matrix
1. SURRE 21
2. CWWK
*Everything Variable with a number suffix belongs to corresponding station listed Back To Station Correlation>>
32. Correlation Matrix
1. SURRE 21
2. SURRE6
*Everything Variable with a number suffix belongs to corresponding station listed Back To Station Correlation>>
33. Correlation Matrix
1. SURRE 21
2. CWMM
*Everything Variable with a number suffix belongs to corresponding station listed Back To Station Correlation>>
34. Correlation Matrix
1. SURRE 21
2. SURRE10
*Everything Variable with a number suffix belongs to corresponding station listed Back To Station Correlation>>
35. Correlation Matrix
1. SURRE 21
2. PITM3
*Daily Rain and Wind Direction Deg are dropped, because more 80% of the data is NA Back To Station Correlation>>
36. Correlation Matrix
1. SURRE 21
2. IBCCOQUI5
*Daily Rain and Wind Direction Deg are dropped, because more 80% of the data is NA Back To Station Correlation>>
37. Correlation Matrix
1. SURRE 21
2. BURNA10
*Daily Rain and Wind Direction Deg are dropped, because more 80% of the data is NA Back To Station Correlation>>