Why does attention to web articles fall with time?

Size: px
Start display at page:

Download "Why does attention to web articles fall with time?"

Transcription

1 Why does attention to web articles fall with time? M.V. Simkin and V.P. Roychowdhury Department of Electrical Engineering, University of California, Los Angeles, CA We analyze access statistics for a few dozen blog entries for a period of several years. Access rate falls as an inverse power of time passed since publication. The power law holds for periods up to thousand days. The exponents are different for different blogs and are distributed between and 3. Decay of attention to aging web articles has been reported before and two explanations were proposed. One explanation introduced some decaying with time novelty factor. Another used some intricate theory of human dynamics. We argue that the decay of attention to a web article is simply caused by the link to it first dropping down the list of links on the website s front page, disappearing from the front page and subsequent movement further into background. Keywords: blogs, internet, statistics, web sites Dezsö et al [] had studied the dynamics of webpage access. Their data source was the access log of one news website. They found that web documents are mostly accessed during first days after their creation, with the number of accesses decreasing with time as a power law n( t) ~ t. They proposed some human dynamics model, which we will discuss later, to explain their result. Wu and Huberman [7] had studied the time series of the number of diggs (bookmarks) on digg.com website. They found that the number of new diggs decreases as the time passed since the story appeared on the website increases. They introduced novelty factor to explain their results. This factor decays as a stretched exponential of the time passed since the story appeared on digg.com. Some webpages show no decay of popularity Let us now have a look at some of our data. Figure shows access statistics for three fixed content webpages from the website reverent.org (there are more examples in Ref. [2]) which are apparently not affected by any decaying novelty factor. The absolute maximum of daily downloads happens two years after webpage publication (Fig. and ) and five years after publication (Fig. {c) ). The mentioned webpages are only two clicks away from site s front page. This assures them decent placing in internet search. For example, during the year 200, 737 internet searches for Donald Judd had led to the webpage in Fig. and 590 searches for famous artist had led to the webpage in Fig. (c). This means that the webpages have some small but constant traffic, directed by search engines. Sometimes visitors mention the webpage that they found in a blog, forum or social networking website. Sometimes a visitor to that blog reposts links in his blog. Sometimes this results in avalanches of blog entries. They lead to spikes of downloads, which are seen in Fig.. We had modeled these avalanches using theory of Branching Processes in Ref. [2]. Therefore, we are not going to repeat the analysis in the present article. One reason why we put Fig. in the article is that it helps to question the novelty factor. Another reason is that it explains how we managed to get access statistics for web articles from many other websites.

2 daily downloads Nov Feb-08 7-Jun-08 5-Sep Dec-08 3-Apr-09 2-Jul Oct Jan-0 8-May-0 0 daily downloads Jan-06 0-Aug Feb-07 4-Sep-07 0-Apr-08 8-Oct May Nov-09 0-Jun daily downloads Jun-04 8-Apr-05 2-Feb-06 9-Dec-06 5-Oct-07 3-Jul May Mar-0 (c) Figure. Access statistics for three webpages: and (c) since the day of their release and until 8/2/200.

3 Referral log allows studying access statistics for many websites When blogs link to the website for which we have the access logs, we can estimate their access statistics from the number of referrals. Obviously, the number of referrals is proportional to the number of visitors to the referring webpage. Figure 2 shows such statistics. We use not calendar days to plot the data, but 24-hr days since first referral. Thus if the first referral occurred at time t on day d, the first 24-hr day includes referrals up to time t on the day d+ and so on. One can see a power law decay of the number of referrals as function of time since link publication y = 4.2x -.34 y = 63.43x y = 2280x y = 60.7x (c) y = 264.3x y = x y = x hr day since the first referral (d) y = x y = x hr day since the first referral Figure 2. Referrals from It at different times linked to two webpages from reverent.org. Although pre-factors are 50% different, the exponents differ only 2%. Referrals from (c) Referrals from which linked to three different pages from reverent.org. Note that it was not a single post linking to three webpages, but three different posts widely separated in time. (d) Referrals from

4 An explanation of the power-law decay of attention The probability that visitors to the webpage follow certain link, posted on this webpage, depends on the position of the link. They follow the current top link with highest probability. The second link they follow with smaller probability than the first and the tens with even smaller probability. One would not expect that position change from first to second would have the same effect as the change from tens to elevens. It would be more natural to assume that proportional decrease in position results in proportional decrease in access probability. So that falling from first to second place reduces access probability by the same factor as falling from the tens place to the twenties. Mathematically this is n( r) r expressed as =. Here n ( r) is the access rate and r is the position rank (so that the top link n( r) r has rank, the second 2 and so on) and some proportionality coefficient. This results in a power law decay of access probability with link s position: n( r) ~ r. We cannot determine the value of the exponent by this reasoning. To do this we need to know by how much the probability to follow a link decreases when its position falls from first to second. For example, if it decreases twice, then the exponent will be exactly. How this relates to time-dependence of access probability? The simplest case is the Reality Carnival site (see Fig. 2). This is a webpage containing links to other webpages, which the owner, Dr. Pickover, found interesting. There is no separate blog entry for each link just the link and a few word description. Dr. Pickover adds one link a day. The new link goes on the top of the list and all already present links fall in their position by. A year worth of links is on the page at a time. Thus, the number of days passed since link addition exactly corresponds to link s position in the list. Therefore, r = t, where t is time passed since link publishing, measure in days. We thus get n t ~ t. ( ) The probability of following a link depends not only on its position in the list, but also on how attractive is its description. The attractiveness factor is constant and does not vary from day to day. Naturally, it influences only a prefactor and not the power law exponent. At different times, Reality Carnival linked to two webpages from reverent.org. One can see from Figure 2 that the prefactors differ.5 times, but exponents are the same within 2%. Similar pattern holds for three other blogs shown in Fig y = 36.03x -.0 referrals per page 00 0 y = 488.5x page number Figure 3. Referrals from The distribution of referrals by page number.

5 y = x referrals y = x Figure 4. Distribution of referrals from by day by page number page number Other blogs are different from the one described: they may add several new items a day, or may add only one item in several days. Great majority of them move earlier entries to next pages. In such case, we can plot the number of referrals as a function of page number. Figures 3 and 4 show such data. The number of referrals falls as a power of the page number. This gives more credence to our claim that the probability of following a link is determined by its position in the website. Discussion of earlier theories Dezsö et al [] had analyzed a month of access log of a Hungarian news website. They reported that the average rate of accessing a news story falls as a power law of the time passed since its publication: n( t) ~ t with = 0.3 ± 0.. They proposed the following theoretical explanation. They found that the distribution of time-intervals τ between the visits by the same visitor follows a power α law p ( τ ) ~ τ with α =.2 ± 0.. They speculated that visitors access all the news items, which appear on the website since their last visit. The number of visitors who did not yet see the document α α of age t is n( t) ~ τ ~ t t, which means that = α. The observed values of α and agree with this theory. There are, however, problems with the above explanation. First, it is not clear from the article what are visitors and what are times between visits. There are two ways of tracing visitors: through cookies and through IP addresses. There is more uncertainty in the definition of a visit. For instance, popular web analytic tool AWStats [3] separates visits when there was over an hour between requests from the same IP. This is quite arbitrary. Therefore, we had to ask the authors what they meant by their words. It turned out [4] that that the visitors where determined from IPs and visits where all HTML requests, that is every line in the access log. This includes not only webpages but also all image files. Thus downloading one webpage with several images produces a number of visits with several intervals between them. That is why the power law in Fig. 4 of Ref. [] spreads into the region of one second intervals between visits. One still could separate real visits: those with interval of a day or more can without doubts called different visits. However, Ref. [] contains no analysis showing that after a long absence a visitor looks at more webpages, than after a short absence. Another concern is that many different users have the same IP: this is certainly a problem studying access log of a major news website of a small country. Another problem arises if we try to apply the theory of Dezsö et al [] to our data. Some of the referrers show power law decay for several years (see Figures 3 and 4). It would be strange to suspect that some users visit with several years intervals and then look up everything they missed.

6 Although the functional form of the frequency of access decay function reported by Dezsö et al [] agrees with our data, the value of the exponent does not. They reported = 0. 3, while we always see >. However, Leskovec et al [6] reported that the average number of new in-links to a blog entry falls of as an inverse power of time passed since publication of this blog entry. The exponent of the power law is.5. We may reason that the number of new in-links is proportional to the number of views (just like the number of referrals). So the findings of Leskovec et al [6] agree with our results. We can also refute the argument [4] that the results of Johansen and Sornette [5] conform to results of Dezsö et al []. Johansen and Sornette [5] studied how the number of downloads of their paper behaved after the url was published in a newspaper. They found that after initial peak the number of downloads fell of as a power law with exponent 0.6. The problem is that they studied the total number of downloads, not the number of referrals from the newspaper. It is certain that the newspaper article trigged a cascade of blog entries linking to the paper. Thus, exponent 0.6 describes not the decay of accessing the newspaper article, but the effect of the whole cascade. We can illustrate this with our data. In Fig. you can see a peak in October It is a result of a cascade triggered by the publication of the link in the popular blog boingboing.net. Figure 5 shows the number of total downloads and the number of referrals from boingboing.net. While the number of downloads relaxes as a power law with exponent 0.9, the number of referrals from boingboing.net falls off with the exponent referrals / total downloads 00 0 y = 54.3x y = 58.95x Figure 5. Rhombs show referrals from boingboing.net, which linked on 0/9/2009 to the webpage whose access statistics is given in Fig. a. Squares show total number of downloads of the webpage in question. Why did Dezsö et al [] observe = 0. 3? To answer the question we first discuss the difference of web articles whose access statistics is shown in Figure from those shown in Figures 2-4. Webpages used in Fig. contribute original content, while those in Figures 2-4 only bring attention to original webpages. When someone reads a blog, which brings attention to an original webpage, and likes that webpage, he always links to the original webpage, and rarely links to the intermediary blog. In contrast, news articles occasionally report interesting events. Thus, some of them can trigger cascades of blog entries, each linking to the original news article. Dezsö et al [] show in their Figure 3 only average data (over almost four thousand news items). We suspect that if the data for separate news stories were available they would look for some news item similar to Figure of the present manuscript. The power law with = 0. 3 is probably an artifact of averaging over many news items with different access patterns.

7 Wu and Huberman [7] had studied the time series of the number of diggs (bookmarks) on digg.com website. They proposed the following model. The evolution of the cumulative number of diggs, N ( t), dn( t) is described by the equation = N( t) r( t) where r( t) is a decay factor. The equation has the dt t solution N( t) = N( 0 ) exp ( ) dt r t. And the number of new diggs is equal to 0 n ( t) ( t) t dn = = N( 0 ) exp dt r( t ) r( t) dt. In the limit of large t, this becomes 0 n ( t) = N( 0) exp dt r( t ) r( t) ~ r( t). They got the best fit to the actual data using the decay factor r t = exp 0.4t. Note that stretched exponential looks very similar to a power law. By looking at ( ) ( ). 5 Figure 3 of Ref. [7] one can guess that ( t) t r = would do almost as good. This agrees well with our data. We suspect that it is not the decaying novelty factor what causes the decay in number of diggs. It is merely a result of the falling of story s position on digg.com website. References. Z. Dezsö, E. Almaas, A. Lukács, B. Rácz, I. Szakadát, and A.-L. Barabási, Dynamics of information access on the web Phys. Rev. E 73, (2006). Also available at: 2. M.V. Simkin, V.P. Roychowdhury, A theory of web traffic Europhysics Letters, 82 (2008) AWStats logfile analyzer 6.9 Documentation 4. Z. Dezsö, private communication 5. A. Johansen and D. Sornette, Download relaxation dynamics on the WWW following newspaper publication of URL Physica A 276 (2000) 338; 6. J. Leskovec, M. McGlohon, C. Faloutsos, N. Glance, M. Hurst Patterns of Cascading Behavior in Large Blog Graphs. Proceedings of the Seventh SIAM International Conference on Data Mining, April 26-28, 2007, Minneapolis, Minnesota, USA F. Wu and B. A. Huberman Novelty and collective attention PNAS 04 (2007) 7599.

GAMINGRE 8/1/ of 7

GAMINGRE 8/1/ of 7 FYE 09/30/92 JULY 92 0.00 254,550.00 0.00 0 0 0 0 0 0 0 0 0 254,550.00 0.00 0.00 0.00 0.00 254,550.00 AUG 10,616,710.31 5,299.95 845,656.83 84,565.68 61,084.86 23,480.82 339,734.73 135,893.89 67,946.95

More information

Computing & Telecommunications Services

Computing & Telecommunications Services Computing & Telecommunications Services Monthly Report September 214 CaTS Help Desk (937) 775-4827 1-888-775-4827 25 Library Annex helpdesk@wright.edu www.wright.edu/cats/ Table of Contents HEAT Ticket

More information

DOZENALS. A project promoting base 12 counting and measuring. Ideas and designs by DSA member (#342) and board member, Timothy F. Travis.

DOZENALS. A project promoting base 12 counting and measuring. Ideas and designs by DSA member (#342) and board member, Timothy F. Travis. R AENBO DOZENALS A project promoting base 12 counting and measuring. Ideas and designs by DSA member (#342) and board member Timothy F. Travis. I became aware as a teenager of base twelve numbering from

More information

WHEN IS IT EVER GOING TO RAIN? Table of Average Annual Rainfall and Rainfall For Selected Arizona Cities

WHEN IS IT EVER GOING TO RAIN? Table of Average Annual Rainfall and Rainfall For Selected Arizona Cities WHEN IS IT EVER GOING TO RAIN? Table of Average Annual Rainfall and 2001-2002 Rainfall For Selected Arizona Cities Phoenix Tucson Flagstaff Avg. 2001-2002 Avg. 2001-2002 Avg. 2001-2002 October 0.7 0.0

More information

ENGINE SERIAL NUMBERS

ENGINE SERIAL NUMBERS ENGINE SERIAL NUMBERS The engine number was also the serial number of the car. Engines were numbered when they were completed, and for the most part went into a chassis within a day or so. However, some

More information

In this activity, students will compare weather data from to determine if there is a warming trend in their community.

In this activity, students will compare weather data from to determine if there is a warming trend in their community. Overview: In this activity, students will compare weather data from 1910-2000 to determine if there is a warming trend in their community. Objectives: The student will: use the Internet to locate scientific

More information

Determine the trend for time series data

Determine the trend for time series data Extra Online Questions Determine the trend for time series data Covers AS 90641 (Statistics and Modelling 3.1) Scholarship Statistics and Modelling Chapter 1 Essent ial exam notes Time series 1. The value

More information

Stochastic modeling of a serial killer

Stochastic modeling of a serial killer This paper appeared in the Journal of Theoretical Biology (24) 355: 6 Stochastic modeling of a serial killer M.V. Simkin and V.P. Roychowdhury Department of Electrical Engineering, University of California,

More information

Computing & Telecommunications Services Monthly Report January CaTS Help Desk. Wright State University (937)

Computing & Telecommunications Services Monthly Report January CaTS Help Desk. Wright State University (937) January 215 Monthly Report Computing & Telecommunications Services Monthly Report January 215 CaTS Help Desk (937) 775-4827 1-888-775-4827 25 Library Annex helpdesk@wright.edu www.wright.edu/cats/ Last

More information

The xmacis Userʼs Guide. Keith L. Eggleston Northeast Regional Climate Center Cornell University Ithaca, NY

The xmacis Userʼs Guide. Keith L. Eggleston Northeast Regional Climate Center Cornell University Ithaca, NY The xmacis Userʼs Guide Keith L. Eggleston Northeast Regional Climate Center Cornell University Ithaca, NY September 22, 2004 Updated September 9, 2008 The xmacis Userʼs Guide The xmacis program consists

More information

Improve Forecasts: Use Defect Signals

Improve Forecasts: Use Defect Signals Improve Forecasts: Use Defect Signals Paul Below paul.below@qsm.com Quantitative Software Management, Inc. Introduction Large development and integration project testing phases can extend over many months

More information

Monitoring on Subsidence Claims. John Parvin Subsidence Claims Manager

Monitoring on Subsidence Claims. John Parvin Subsidence Claims Manager Monitoring on Subsidence Claims John Parvin Subsidence Claims Manager Key Milestones Subsidence cover 1972 Surge of claims1989/1990/1991 Project Management 1992 onwards Mitigation Surge 1995/2003 Delegated

More information

DEPARTMENT OF THE ARMY MILITARY SURFACE DEPLOYMENT AND DISTRIBUTION COMMAND (SDDC) 1 SOLDIER WAY SCOTT AFB, IL 62225

DEPARTMENT OF THE ARMY MILITARY SURFACE DEPLOYMENT AND DISTRIBUTION COMMAND (SDDC) 1 SOLDIER WAY SCOTT AFB, IL 62225 DEPARTMENT OF THE ARMY MILITARY SURFACE DEPLOYMENT AND DISTRIBUTION COMMAND (SDDC) 1 SOLDIER WAY SCOTT AFB, IL 62225 SDDC Operations Special Requirements Branch 1 Soldier Way Scott AFB, IL 62225 April

More information

Investigating Factors that Influence Climate

Investigating Factors that Influence Climate Investigating Factors that Influence Climate Description In this lesson* students investigate the climate of a particular latitude and longitude in North America by collecting real data from My NASA Data

More information

Climatography of the United States No

Climatography of the United States No Climate Division: AK 5 NWS Call Sign: ANC Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 90 Number of s (3) Jan 22.2 9.3 15.8

More information

SO x is a cubed root of t

SO x is a cubed root of t 7.6nth Roots 1) What do we know about x because of the following equation x 3 = t? All in one.docx SO x is a cubed root of t 2) Definition of nth root: 3) Study example 1 4) Now try the following problem

More information

Drought in Southeast Colorado

Drought in Southeast Colorado Drought in Southeast Colorado Nolan Doesken and Roger Pielke, Sr. Colorado Climate Center Prepared by Tara Green and Odie Bliss http://climate.atmos.colostate.edu 1 Historical Perspective on Drought Tourism

More information

DAILY QUESTIONS 28 TH JUNE 18 REASONING - CALENDAR

DAILY QUESTIONS 28 TH JUNE 18 REASONING - CALENDAR DAILY QUESTIONS 28 TH JUNE 18 REASONING - CALENDAR LEAP AND NON-LEAP YEAR *A non-leap year has 365 days whereas a leap year has 366 days. (as February has 29 days). *Every year which is divisible by 4

More information

Time Series Analysis

Time Series Analysis Time Series Analysis A time series is a sequence of observations made: 1) over a continuous time interval, 2) of successive measurements across that interval, 3) using equal spacing between consecutive

More information

Monitoring Platelet Issues - a novel approach CUSUM. Clive Hyam Blood Stocks Management Scheme London

Monitoring Platelet Issues - a novel approach CUSUM. Clive Hyam Blood Stocks Management Scheme London Monitoring Platelet Issues - a novel approach CUSUM Clive Hyam Blood Stocks Management Scheme London Overview of Presentation What s driving the need to better understand platelet issues Potential tools

More information

S95 INCOME-TESTED ASSISTANCE RECONCILIATION WORKSHEET (V3.1MF)

S95 INCOME-TESTED ASSISTANCE RECONCILIATION WORKSHEET (V3.1MF) Welcome! Here's your reconciliation Quick-Start. Please read all five steps before you get started. 1 2 3 Excel 2003? Are you using software other than Microsoft Excel 2003? Say what? Here are the concepts

More information

Annual Average NYMEX Strip Comparison 7/03/2017

Annual Average NYMEX Strip Comparison 7/03/2017 Annual Average NYMEX Strip Comparison 7/03/2017 To Year to Year Oil Price Deck ($/bbl) change Year change 7/3/2017 6/1/2017 5/1/2017 4/3/2017 3/1/2017 2/1/2017-2.7% 2017 Average -10.4% 47.52 48.84 49.58

More information

Lesson Adaptation Activity: Analyzing and Interpreting Data

Lesson Adaptation Activity: Analyzing and Interpreting Data Lesson Adaptation Activity: Analyzing and Interpreting Data Related MA STE Framework Standard: 3-ESS2-1. Use graphs and tables of local weather data to describe and predict typical weather during a particular

More information

SYSTEM BRIEF DAILY SUMMARY

SYSTEM BRIEF DAILY SUMMARY SYSTEM BRIEF DAILY SUMMARY * ANNUAL MaxTemp NEL (MWH) Hr Ending Hr Ending LOAD (PEAK HOURS 7:00 AM TO 10:00 PM MON-SAT) ENERGY (MWH) INCREMENTAL COST DAY DATE Civic TOTAL MAXIMUM @Max MINIMUM @Min FACTOR

More information

Your World is not Red or Green. Good Practice in Data Display and Dashboard Design

Your World is not Red or Green. Good Practice in Data Display and Dashboard Design Your World is not Red or Green Good Practice in Data Display and Dashboard Design References Tufte, E. R. (2). The visual display of quantitative information (2nd Ed.). Cheshire, CT: Graphics Press. Few,

More information

Calculations Equation of Time. EQUATION OF TIME = apparent solar time - mean solar time

Calculations Equation of Time. EQUATION OF TIME = apparent solar time - mean solar time Calculations Equation of Time APPARENT SOLAR TIME is the time that is shown on sundials. A MEAN SOLAR DAY is a constant 24 hours every day of the year. Apparent solar days are measured from noon one day

More information

GRADE 6 GEOGRAPHY TERM 1 LATITUDE AND LONGITUDE (degrees)

GRADE 6 GEOGRAPHY TERM 1 LATITUDE AND LONGITUDE (degrees) 1 GRADE 6 GEOGRAPHY TERM 1 LATITUDE AND LONGITUDE (degrees) Contents Lines of Latitude... 2 Lines of Longitude... 3 The hemispheres of The Earth... 4 Finding countries and cities on a map using latitude

More information

Meteorological Data recorded at Armagh Observatory from 1795 to 2001: Volume I - Daily, Monthly and Annual Rainfall

Meteorological Data recorded at Armagh Observatory from 1795 to 2001: Volume I - Daily, Monthly and Annual Rainfall Meteorological Data recorded at Armagh Observatory from 1795 to 2001: Volume I - Daily, Monthly and Annual Rainfall 1838-2001 A. M. García-Suárez, C.J. Butler, D. Cardwell, A.D.S. Coughlin, A. Donnelly,

More information

Pre-Calc Chapter 1 Sample Test. D) slope: 3 4

Pre-Calc Chapter 1 Sample Test. D) slope: 3 4 Pre-Calc Chapter 1 Sample Test 1. Use the graphs of f and g to evaluate the function. f( x) gx ( ) (f o g)(-0.5) 1 1 0 4. Plot the points and find the slope of the line passing through the pair of points.

More information

THE LIGHT SIDE OF TRIGONOMETRY

THE LIGHT SIDE OF TRIGONOMETRY MATHEMATICAL METHODS: UNIT 2 APPLICATION TASK THE LIGHT SIDE OF TRIGONOMETRY The earth s movement around the sun is an example of periodic motion. The earth s tilt on its axis and corresponding movement

More information

Contents. Histograms and the Mean Hand Spans 25 Fathers and Sons Revisited 26 Water 28 Sun and Snow 29 Summary 32 Check Your Work 32

Contents. Histograms and the Mean Hand Spans 25 Fathers and Sons Revisited 26 Water 28 Sun and Snow 29 Summary 32 Check Your Work 32 Contents Section D Hand Spans 25 Fathers and Sons Revisited 26 Water 28 Sun and Snow 29 Summary 32 Check Your Work 32 Additional Practice Answers to Check Your Work Student Activity Sheets Contents v D

More information

Climatography of the United States No

Climatography of the United States No Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 100 Number of s (3) Jan 63.9 39.3 51.6 86 1976 16 56.6 1986 20 1976 2 47.5 1973

More information

Climatography of the United States No

Climatography of the United States No Temperature ( F) Month (1) Min (2) Month(1) Extremes Lowest (2) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 100 Number of s (3) Jan 32.8 21.7 27.3 62 1918 1 35.8 1983-24 1950 29 10.5 1979

More information

Mr. XYZ. Stock Market Trading and Investment Astrology Report. Report Duration: 12 months. Type: Both Stocks and Option. Date: Apr 12, 2011

Mr. XYZ. Stock Market Trading and Investment Astrology Report. Report Duration: 12 months. Type: Both Stocks and Option. Date: Apr 12, 2011 Mr. XYZ Stock Market Trading and Investment Astrology Report Report Duration: 12 months Type: Both Stocks and Option Date: Apr 12, 2011 KT Astrologer Website: http://www.softwareandfinance.com/magazine/astrology/kt_astrologer.php

More information

TMC Monthly Operational Summary

TMC Monthly Operational Summary TMC Monthly Operational Summary July 1 Bureau of Transportation Systems Management & Operations (TSMO) NH Department of Transportation s Mission Transportation excellence enhancing the quality of life

More information

AdvAlg9.7LogarithmsToBasesOtherThan10.notebook. March 08, 2018

AdvAlg9.7LogarithmsToBasesOtherThan10.notebook. March 08, 2018 AdvAlg9.7LogarithmsToBasesOtherThan10.notebook In order to isolate a variable within a logarithm of an equation, you need to re write the equation as the equivalent exponential equation. In order to isolate

More information

MISSION DEBRIEFING: Teacher Guide

MISSION DEBRIEFING: Teacher Guide Activity 2: It s Raining Again?! Using real data from one particular location, students will interpret a graph that relates rainfall to the number of cases of malaria. Background The relationship between

More information

Finding Aid for the Collection of Material about the Southern Pacific Railway,

Finding Aid for the Collection of Material about the Southern Pacific Railway, http://oac.cdlib.org/findaid/ark:/13030/kt0779p30k No online items Pacific Railway, 1900-1950 Processed by UCLA Library Special Collections staff; machine-readable finding aid created by Caroline Cubé.

More information

Climatography of the United States No

Climatography of the United States No Climate Division: CA 4 NWS Call Sign: Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 100 Number of s (3) Jan 55.6 39.3 47.5 77

More information

Climatography of the United States No

Climatography of the United States No Climate Division: CA 1 NWS Call Sign: Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 100 Number of s (3) Jan 57.9 38.9 48.4 85

More information

Climatography of the United States No

Climatography of the United States No Climate Division: CA 5 NWS Call Sign: Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 100 Number of s (3) Jan 56.6 36.5 46.6 81

More information

Climatography of the United States No

Climatography of the United States No Climate Division: CA 5 NWS Call Sign: Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 100 Number of s (3) Jan 44.8 25.4 35.1 72

More information

Climatography of the United States No

Climatography of the United States No Climate Division: CA 4 NWS Call Sign: Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 100 Number of s (3) Jan 49.4 37.5 43.5 73

More information

Climatography of the United States No

Climatography of the United States No Climate Division: CA 6 NWS Call Sign: Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 100 Number of s (3) Jan 69.4 46.6 58.0 92

More information

Climatography of the United States No

Climatography of the United States No Climate Division: CA 4 NWS Call Sign: Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 1 Number of s (3) Jan 58.5 38.8 48.7 79 1962

More information

Climatography of the United States No

Climatography of the United States No Climate Division: CA 6 NWS Call Sign: Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 1 Number of s (3) Jan 67.5 42. 54.8 92 1971

More information

Climatography of the United States No

Climatography of the United States No Climate Division: CA 1 NWS Call Sign: Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 1 Number of s (3) Jan 57.8 39.5 48.7 85 1962

More information

Outage Coordination and Business Practices

Outage Coordination and Business Practices Outage Coordination and Business Practices 1 2007 Objectives What drove the need for developing a planning/coordination process. Why outage planning/coordination is crucial and important. Determining what

More information

DOWNLOAD OR READ : THE YEARLY SON SHINE JOURNAL PDF EBOOK EPUB MOBI

DOWNLOAD OR READ : THE YEARLY SON SHINE JOURNAL PDF EBOOK EPUB MOBI DOWNLOAD OR READ : THE YEARLY SON SHINE JOURNAL PDF EBOOK EPUB MOBI Page 1 Page 2 the yearly son shine journal the yearly son shine pdf the yearly son shine journal Like the page, https://www.facebook.com/fscguides

More information

Jackson County 2013 Weather Data

Jackson County 2013 Weather Data Jackson County 2013 Weather Data 61 Years of Weather Data Recorded at the UF/IFAS Marianna North Florida Research and Education Center Doug Mayo Jackson County Extension Director 1952-2008 Rainfall Data

More information

Climatography of the United States No

Climatography of the United States No Climate Division: ND 8 NWS Call Sign: BIS Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 100 Number of s (3) Jan 21.1 -.6 10.2

More information

JANUARY MONDAY TUESDAY WEDNESDAY THURSDAY FRIDAY SATURDAY SUNDAY

JANUARY MONDAY TUESDAY WEDNESDAY THURSDAY FRIDAY SATURDAY SUNDAY Vocabulary (01) The Calendar (012) In context: Look at the calendar. Then, answer the questions. JANUARY MONDAY TUESDAY WEDNESDAY THURSDAY FRIDAY SATURDAY SUNDAY 1 New 2 3 4 5 6 Year s Day 7 8 9 10 11

More information

Climatography of the United States No

Climatography of the United States No Climate Division: TN 1 NWS Call Sign: Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 100 Number of s (3) Jan 47.6 24.9 36.3 81

More information

Climatography of the United States No

Climatography of the United States No Climate Division: CA 5 NWS Call Sign: FAT Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 1 Number of s (3) Jan 53.6 38.4 46. 78

More information

BRADSHAW'S RAILWAY GUIDE : accessible copies

BRADSHAW'S RAILWAY GUIDE : accessible copies BRADSHAW'S RAILWAY GUIDE : accessible copies Y = copy held; YS = copy held with supplement; R = reprint held; I = incomplete copy held; F = fragile copy (not available for general public - access limited);

More information

SEO & Marketing Report: Rank & Traffic (Monthly Comprehensive)

SEO & Marketing Report: Rank & Traffic (Monthly Comprehensive) SEO & Marketing Report: & Traffic ( Comprehensive) 06/15/2015 Domain Statistics > Domain Analysis Keyword Performance Primary Domain Keyword Performance Competition Analysis Primary Domain vs. Competitor

More information

Climatography of the United States No

Climatography of the United States No Climate Division: CA 6 NWS Call Sign: 1L2 N Lon: 118 3W Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 1 Number of s (3) Jan 63.7

More information

Climatography of the United States No

Climatography of the United States No Climate Division: CA 5 NWS Call Sign: BFL Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 1 Number of s (3) Jan 56.3 39.3 47.8

More information

SYSTEM BRIEF DAILY SUMMARY

SYSTEM BRIEF DAILY SUMMARY SYSTEM BRIEF DAILY SUMMARY * ANNUAL MaxTemp NEL (MWH) Hr Ending Hr Ending LOAD (PEAK HOURS 7:00 AM TO 10:00 PM MON-SAT) ENERGY (MWH) INCREMENTAL COST DAY DATE Civic TOTAL MAXIMUM @Max MINIMUM @Min FACTOR

More information

FEB DASHBOARD FEB JAN FEB MAR APR MAY JUN JUL AUG SEP OCT NOV DEC

FEB DASHBOARD FEB JAN FEB MAR APR MAY JUN JUL AUG SEP OCT NOV DEC Positive Response Compliance 215 Compliant 215 Non-Compliant 216 Compliant 216 Non-Compliant 1% 87% 96% 86% 96% 88% 89% 89% 88% 86% 92% 93% 94% 96% 94% 8% 6% 4% 2% 13% 4% 14% 4% 12% 11% 11% 12% JAN MAR

More information

TMC Monthly Operational Summary

TMC Monthly Operational Summary TMC Monthly Operational Summary March Bureau of Transportation Systems Management & Operations (TSMO) NH Department of Transportation s Mission Transportation excellence enhancing the quality of life in

More information

What is the difference between Weather and Climate?

What is the difference between Weather and Climate? What is the difference between Weather and Climate? Objective Many people are confused about the difference between weather and climate. This makes understanding the difference between weather forecasts

More information

Climatography of the United States No

Climatography of the United States No Climate Division: TN 3 NWS Call Sign: BNA Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 100 Number of s (3) Jan 45.6 27.9 36.8

More information

2013 Tide Newsletter and occasionally by much more. What's more,

2013 Tide Newsletter and occasionally by much more. What's more, The Official Newsletter for the Nor easters Metal Detecting Club! Tide s Ed it io n HTTP://WWW.NOR EASTER S.NET Year ly Ti des for 2013 The Metal Detecting Creed By Jessie Thompson We are Metal Detectorists.

More information

Climatography of the United States No

Climatography of the United States No Climate Division: CA 5 NWS Call Sign: Elevation: 6 Feet Lat: 37 Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 1 Number of s (3)

More information

Climatography of the United States No

Climatography of the United States No Climate Division: CA 4 NWS Call Sign: Elevation: 2 Feet Lat: 37 Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 1 Number of s (3)

More information

Climatography of the United States No

Climatography of the United States No Climate Division: CA 4 NWS Call Sign: Elevation: 13 Feet Lat: 36 Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 1 Number of s

More information

Climatography of the United States No

Climatography of the United States No Climate Division: CA 5 NWS Call Sign: Elevation: 1,14 Feet Lat: 36 Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 1 Number of

More information

Forecasting the Canadian Dollar Exchange Rate Wissam Saleh & Pablo Navarro

Forecasting the Canadian Dollar Exchange Rate Wissam Saleh & Pablo Navarro Forecasting the Canadian Dollar Exchange Rate Wissam Saleh & Pablo Navarro Research Question: What variables effect the Canadian/US exchange rate? Do energy prices have an effect on the Canadian/US exchange

More information

Identification of Bursts in a Document Stream

Identification of Bursts in a Document Stream Identification of Bursts in a Document Stream Toshiaki FUJIKI 1, Tomoyuki NANNO 1, Yasuhiro SUZUKI 1 and Manabu OKUMURA 2 1 Interdisciplinary Graduate School of Science and Engineering, Tokyo Institute

More information

Time Series Analysis of United States of America Crude Oil and Petroleum Products Importations from Saudi Arabia

Time Series Analysis of United States of America Crude Oil and Petroleum Products Importations from Saudi Arabia International Journal of Applied Science and Technology Vol. 5, No. 5; October 2015 Time Series Analysis of United States of America Crude Oil and Petroleum Products Importations from Saudi Arabia Olayan

More information

Climatography of the United States No

Climatography of the United States No Climate Division: CA 6 NWS Call Sign: LAX Elevation: 1 Feet Lat: 33 Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 1 Number of

More information

Whitby Community College Your account expires on: 8 Nov, 2015

Whitby Community College Your account expires on: 8 Nov, 2015 To print higher resolution math symbols, click the Hi Res Fonts for Printing button on the jsmath control panel. If the math symbols print as black boxes, turn off image alpha channels using the Options

More information

Climatography of the United States No

Climatography of the United States No Climate Division: CA 6 NWS Call Sign: TOA Elevation: 11 Feet Lat: 33 2W Temperature ( F) Month (1) Min (2) Month(1) Extremes Lowest (2) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 1 Number

More information

Chapter 1 Handout: Descriptive Statistics

Chapter 1 Handout: Descriptive Statistics Preview Chapter 1 Handout: Descriptive Statistics Describing a Single Data Variable o Introduction to Distributions o Measure of the Distribution Center: Mean (Average) o Measures of the Distribution Spread:

More information

CE394k.3 - ArcGIS in Water Resources Term Project Update, Fall 2012

CE394k.3 - ArcGIS in Water Resources Term Project Update, Fall 2012 CE394k.3 - ArcGIS in Water Resources Term Project Update, Fall 2012 Project Description: Prepared by Nick Brethorst October 29, 2012 ArcGIS Mapping of the Six Basins Watershed in, CA The Six Basins refers

More information

Introduction to Forecasting

Introduction to Forecasting Introduction to Forecasting Introduction to Forecasting Predicting the future Not an exact science but instead consists of a set of statistical tools and techniques that are supported by human judgment

More information

Average 175, , , , , , ,046 YTD Total 1,098,649 1,509,593 1,868,795 1,418, ,169 1,977,225 2,065,321

Average 175, , , , , , ,046 YTD Total 1,098,649 1,509,593 1,868,795 1,418, ,169 1,977,225 2,065,321 AGRICULTURE 01-Agriculture JUL 2,944-4,465 1,783-146 102 AUG 2,753 6,497 5,321 1,233 1,678 744 1,469 SEP - 4,274 4,183 1,596 - - 238 OCT 2,694 - - 1,032 340-276 NOV 1,979-5,822 637 3,221 1,923 1,532 DEC

More information

Average 175, , , , , , ,940 YTD Total 944,460 1,284,944 1,635,177 1,183, ,954 1,744,134 1,565,640

Average 175, , , , , , ,940 YTD Total 944,460 1,284,944 1,635,177 1,183, ,954 1,744,134 1,565,640 AGRICULTURE 01-Agriculture JUL 2,944-4,465 1,783-146 102 AUG 2,753 6,497 5,321 1,233 1,678 744 1,469 SEP - 4,274 4,183 1,596 - - 238 OCT 2,694 - - 1,032 340-276 NOV 1,979-5,822 637 3,221 1,923 1,532 DEC

More information

Climatography of the United States No

Climatography of the United States No No. 2 1971-2 Asheville, North Carolina 2881 COOP ID: 46646 Climate Division: CA 4 NWS Call Sign: 8W Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp

More information

What Does It Take to Get Out of Drought?

What Does It Take to Get Out of Drought? What Does It Take to Get Out of Drought? Nolan J. Doesken Colorado Climate Center Colorado State University http://ccc.atmos.colostate.edu Presented at the Insects, Diseases and Drought Workshop, May 19,

More information

Climatography of the United States No

Climatography of the United States No No. 2 1971-2 Asheville, North Carolina 2881 COOP ID: 4792 Climate Division: CA 6 NWS Call Sign: Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65

More information

EXAMINATIONS OF THE ROYAL STATISTICAL SOCIETY

EXAMINATIONS OF THE ROYAL STATISTICAL SOCIETY EXAMINATIONS OF THE ROYAL STATISTICAL SOCIETY GRADUATE DIPLOMA, 011 MODULE 3 : Stochastic processes and time series Time allowed: Three Hours Candidates should answer FIVE questions. All questions carry

More information

Jure Leskovec Stanford University

Jure Leskovec Stanford University Jure Leskovec Stanford University 2 Part 1: Models for networks Part 2: Information flows in networks Information spread in social media 3 Information flows through networks Analyzing underlying mechanisms

More information

Chiang Rai Province CC Threat overview AAS1109 Mekong ARCC

Chiang Rai Province CC Threat overview AAS1109 Mekong ARCC Chiang Rai Province CC Threat overview AAS1109 Mekong ARCC This threat overview relies on projections of future climate change in the Mekong Basin for the period 2045-2069 compared to a baseline of 1980-2005.

More information

AREP GAW. AQ Forecasting

AREP GAW. AQ Forecasting AQ Forecasting What Are We Forecasting Averaging Time (3 of 3) PM10 Daily Maximum Values, 2001 Santiago, Chile (MACAM stations) 300 Level 2 Pre-Emergency Level 1 Alert 200 Air Quality Standard 150 100

More information

Climatography of the United States No

Climatography of the United States No No. 2 1971-2 Asheville, North Carolina 2881 COOP ID: 43417 Climate Division: CA 4 NWS Call Sign: N Lon: 121 Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1)

More information

PRELIMINARY DRAFT FOR DISCUSSION PURPOSES

PRELIMINARY DRAFT FOR DISCUSSION PURPOSES Memorandum To: David Thompson From: John Haapala CC: Dan McDonald Bob Montgomery Date: February 24, 2003 File #: 1003551 Re: Lake Wenatchee Historic Water Levels, Operation Model, and Flood Operation This

More information

Tracking Accuracy: An Essential Step to Improve Your Forecasting Process

Tracking Accuracy: An Essential Step to Improve Your Forecasting Process Tracking Accuracy: An Essential Step to Improve Your Forecasting Process Presented by Eric Stellwagen President & Co-founder Business Forecast Systems, Inc. estellwagen@forecastpro.com Business Forecast

More information

2003 Water Year Wrap-Up and Look Ahead

2003 Water Year Wrap-Up and Look Ahead 2003 Water Year Wrap-Up and Look Ahead Nolan Doesken Colorado Climate Center Prepared by Odie Bliss http://ccc.atmos.colostate.edu Colorado Average Annual Precipitation Map South Platte Average Precipitation

More information

Climatography of the United States No

Climatography of the United States No No. 2 1971-2 Asheville, North Carolina 2881 COOP ID: 4795 Climate Division: CA 6 NWS Call Sign: SBA Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp

More information

NatGasWeather.com Daily Report

NatGasWeather.com Daily Report NatGasWeather.com Daily Report Issue Time: 5:15 pm EST Sunday, February 28 th, 2016 for Monday, Feb 29 th 7-Day Weather Summary (February 28 th March 5 th ): High pressure will dominate much of the US

More information

Cambridge International Examinations Cambridge International Advanced Subsidiary and Advanced Level

Cambridge International Examinations Cambridge International Advanced Subsidiary and Advanced Level Cambridge International Examinations Cambridge International Advanced Subsidiary and Advanced Level *2554656732* MARINE SCIENCE 9693/01 Paper 1 AS Structured Questions October/November 2017 1 hour 30 minutes

More information

Climatography of the United States No

Climatography of the United States No Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 100 Number of s (3) 42.6 24.2 33.4 79 1950 25 44.2 1974-16 1994 19 18.8 1977 977

More information

Jackson County 2018 Weather Data 67 Years of Weather Data Recorded at the UF/IFAS Marianna North Florida Research and Education Center

Jackson County 2018 Weather Data 67 Years of Weather Data Recorded at the UF/IFAS Marianna North Florida Research and Education Center Jackson County 2018 Weather Data 67 Years of Weather Data Recorded at the UF/IFAS Marianna North Florida Research and Education Center Doug Mayo Jackson County Extension Director 1952-2008 Rainfall Data

More information

Climatography of the United States No

Climatography of the United States No No. 2 1971-2 Asheville, North Carolina 2881 COOP ID: 46175 Climate Division: CA 6 NWS Call Sign: 3L3 Elevation: 1 Feet Lat: 33 Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1)

More information

Climatography of the United States No

Climatography of the United States No No. 2 1971-2 Asheville, North Carolina 2881 COOP ID: 42713 Climate Division: CA 7 NWS Call Sign: Elevation: -3 Feet Lat: 32 Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1)

More information

Weather History on the Bishop Paiute Reservation

Weather History on the Bishop Paiute Reservation Weather History on the Bishop Paiute Reservation -211 For additional information contact Toni Richards, Air Quality Specialist 76 873 784 toni.richards@bishoppaiute.org Updated 2//214 3:14 PM Weather History

More information

Process Behavior Analysis Understanding Variation

Process Behavior Analysis Understanding Variation Process Behavior Analysis Understanding Variation Steven J Mazzuca ASQ 2015-11-11 Why Process Behavior Analysis? Every day we waste valuable resources because we misunderstand or misinterpret what our

More information

Integrating Weather Forecasts into Folsom Reservoir Operations

Integrating Weather Forecasts into Folsom Reservoir Operations Integrating Weather Forecasts into Folsom Reservoir Operations California Extreme Precipitation Symposium September 6, 2016 Brad Moore, PE US Army Corps of Engineers Biography Brad Moore is a Lead Civil

More information