{"id":986,"date":"2022-09-14T00:51:28","date_gmt":"2022-09-14T07:51:28","guid":{"rendered":"https:\/\/radwatch.berkeley.edu\/?p=986"},"modified":"2022-09-27T21:38:20","modified_gmt":"2022-09-28T04:38:20","slug":"dosenet-summer-2022-vikram-gills-report","status":"publish","type":"post","link":"https:\/\/radwatch.berkeley.edu\/es\/2022\/09\/dosenet-summer-2022-vikram-gills-report\/","title":{"rendered":"DoseNet Summer 2022: Vikram Gill&#8217;s Report"},"content":{"rendered":"<p><b>Introduction<\/b><\/p>\n<p><span style=\"font-weight: 400;\">My work for the 2022 summer semester consisted of analyzing the accuracy of DoseNet\u2019s sensors with comparisons to nearby sensors on the WeatherUnderground network. Accuracy and correlations were the main themes of my project, using linear regression models and t-tests to measure correlations between datasets.\u00a0<\/span><\/p>\n<p>&nbsp;<\/p>\n<p><b>Data Acquisition<\/b><\/p>\n<p><span style=\"font-weight: 400;\">Weather data was sourced from various DoseNet sensors (Figure 1), paired with nearby sensors on WeatherUnderground\u2019s network (weatherunderground.com). Due to long element load times on the website, Selenium webdriver\u2019s were used to extract the element containing the weather data. The data was then saved into an html file that was reformatted into a Pandas DataFrame through the <\/span><i><span style=\"font-weight: 400;\">read_html<\/span><\/i><span style=\"font-weight: 400;\"> method. Using Pandas\u2019 built in <\/span><i><span style=\"font-weight: 400;\">str.replace<\/span><\/i><span style=\"font-weight: 400;\">, .<\/span><i><span style=\"font-weight: 400;\">astype, and .rename<\/span><\/i><span style=\"font-weight: 400;\">, I was able to clear the DataFrame of typographical symbols. This data was ready to be put into a linear regression model and used in calculations.<\/span><\/p>\n<p style=\"text-align: center;\"><b>\u00a0<\/b><\/p>\n<p><span style=\"font-weight: 400;\">DoseNet sensors (i.e. Etcheverry Roof) gather data at five minute intervals, often deviating 1-2 minutes from WeatherUnderground\u2019s readings. This was often acceptable for simple tasks such as comparing readings for temperature between the two sensors. For more complex tasks (i.e. comparing precipitation or Csl data) it was necessary to have well-formatted data. Binning the data using Pandas resampling (for our analysis, we used 5 minutes) allowed for equal time distributions which fulfilled this requirement.\u00a0<\/span><\/p>\n<p style=\"text-align: center;\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-992\" src=\"https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/Screen-Shot-2022-09-14-at-1.10.05-AM.png\" alt=\"\" width=\"495\" height=\"362\" \/><\/p>\n<p><b>Analysis and Results<\/b><\/p>\n<p><span style=\"font-weight: 400;\">To analyze the data gathered, I had to determine the best statistical measures for the limited information available and the distinct groups of data. For the purpose of extracting correlations, I found a linear regression model to work best. Paired with a t-test, I would have a good idea of the relative correlation between any two compared variables. My experiments started with the comparison readings between the \u2018Etcheverry Roof\u2019 and \u2018NearEtch\u2019 temperature sensors (Figure 1). When displaying the data sets in a linear regression model using Sci-Kit Learn\u2019s <\/span><i><span style=\"font-weight: 400;\">LinearRegressor <\/span><\/i><span style=\"font-weight: 400;\">function, it was apparent that there was a slight variation between the two datasets (Figure 2a).\u00a0 The t-test result, \u2018T-value\u2019, indicated that there was no statistically significant difference between the datasets (Figure 3, Figure 4), further supporting that there are only slight variations between the measurements. Similar results were seen for humidity and pressure measurements (Figure 2b, Figure 2c).<\/span><\/p>\n<p><b><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-993 aligncenter\" src=\"https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_2a_Etch_Temp_06_08.png\" alt=\"\" width=\"295\" height=\"185\" \/><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-994 aligncenter\" src=\"https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_2b_Etch_Humidity_06_08.png\" alt=\"\" width=\"280\" height=\"186\" srcset=\"https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_2b_Etch_Humidity_06_08.png 576w, https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_2b_Etch_Humidity_06_08-300x200.png 300w, https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_2b_Etch_Humidity_06_08-272x182.png 272w\" sizes=\"auto, (max-width: 280px) 100vw, 280px\" \/> <img loading=\"lazy\" decoding=\"async\" class=\"wp-image-995 aligncenter\" src=\"https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_2c_Etch_Pressure_06_08.png\" alt=\"\" width=\"287\" height=\"183\" \/><\/b><\/p>\n<p>&nbsp;<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-996 size-full\" src=\"https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_3_tval-e1663144013196.png\" alt=\"\" width=\"581\" height=\"281\" srcset=\"https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_3_tval-e1663144013196.png 581w, https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_3_tval-e1663144013196-300x145.png 300w\" sizes=\"auto, (max-width: 581px) 100vw, 581px\" \/><\/p>\n<p>&nbsp;<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-1004 size-full aligncenter\" src=\"https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/Findings-4-e1663228362632.png\" alt=\"\" width=\"586\" height=\"304\" srcset=\"https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/Findings-4-e1663228362632.png 586w, https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/Findings-4-e1663228362632-300x156.png 300w\" sizes=\"auto, (max-width: 586px) 100vw, 586px\" \/><\/p>\n<p><span style=\"font-weight: 400;\">With the null hypothesis as \u2018no difference\u2019, the calculated p-values (Figure 4), all significantly higher than 0.05, indicate a very strong correlation between the DoseNet and WeatherUnderground temperature\/humidity\/pressure sensors.<\/span><\/p>\n<p>&nbsp;<\/p>\n<p><span style=\"font-weight: 400;\">It is reasonable to assume any variations found could, in part, be due to differences in sensor conditions. These results were reflected in the rest of the sensor comparisons.\u00a0<\/span><\/p>\n<p>&nbsp;<\/p>\n<p><span style=\"font-weight: 400;\">Using this template, I tackled unusual readings from precipitation (Decrisp) sensors at LBL. The sensor, working on a scale of 0-10, reported readings with no clear source. Initially, I compared the precipitation readings to precipitation data from WeatherUnderground, but no clear variation in the data was found. Any spikes were drowned out by \u2018zero\u2019 readings (Figure 5). No t-value or p-value was taken into consideration due to the overwhelming amount of equivalent \u2018zero\u2019 data (this indication of correlation would not be helpful.) Similar was found when comparing raw data, as WeatherUnderground\u2019s sensors reported no accumulation of precipitation.<\/span><\/p>\n<p><span style=\"font-weight: 400;\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-1002 size-full aligncenter\" src=\"https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_5_LBL_NEARLBL_RAIN.png\" alt=\"\" width=\"576\" height=\"384\" srcset=\"https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_5_LBL_NEARLBL_RAIN.png 576w, https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_5_LBL_NEARLBL_RAIN-300x200.png 300w, https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_5_LBL_NEARLBL_RAIN-272x182.png 272w\" sizes=\"auto, (max-width: 576px) 100vw, 576px\" \/><\/span><\/p>\n<p><span style=\"font-weight: 400;\">However, raw data indicated some similar spikes in wind speed data from WeatherUnderground to the perception readings. (Figure 6a) Although, plotting the data did not show any direct correlation, and t-values (Figure 6b) must be looked at with skepticism, as their only purpose here is to quantify slight departure from expected values<\/span><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-999 size-full aligncenter\" src=\"https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_6_LBL_NEARLBL_SPEED.png\" alt=\"\" width=\"576\" height=\"384\" srcset=\"https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_6_LBL_NEARLBL_SPEED.png 576w, https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_6_LBL_NEARLBL_SPEED-300x200.png 300w, https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_6_LBL_NEARLBL_SPEED-272x182.png 272w\" sizes=\"auto, (max-width: 576px) 100vw, 576px\" \/><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-1000 aligncenter\" src=\"https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_6b_LBL_NEARLBL_SPEED-e1663227330903.png\" alt=\"\" width=\"447\" height=\"161\" srcset=\"https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_6b_LBL_NEARLBL_SPEED-e1663227330903.png 400w, https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_6b_LBL_NEARLBL_SPEED-e1663227330903-300x108.png 300w\" sizes=\"auto, (max-width: 447px) 100vw, 447px\" \/><\/p>\n<p><span style=\"font-weight: 400;\">While there is no conclusive statement for the precipitation phenomenon, it\u2019s safe to say that it is not correlated with rain readings from other nearby sensors.\u00a0<\/span><\/p>\n<p><b>Conclusion<\/b><\/p>\n<p><span style=\"font-weight: 400;\">Through the statistically significant correlation between the Temperature\/Humidity\/Pressure sensors of the DoseNet and WeatherUnderground sensors, we can conclude that they\u2019re highly accurate. As we found, the p-value was nearly 1, and the t-value was nearly 0, both supporting the strong correlation. From earlier tests (Figure 7a, Figure 7b) for accuracy between WeatherUnderground stations situated about a block away from each other, slight variations were expected. <\/span><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-1001 aligncenter\" src=\"https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_7a_WU_ACCURACY_193_187_060822.png\" alt=\"\" width=\"374\" height=\"249\" srcset=\"https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_7a_WU_ACCURACY_193_187_060822.png 576w, https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_7a_WU_ACCURACY_193_187_060822-300x200.png 300w, https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_7a_WU_ACCURACY_193_187_060822-272x182.png 272w\" sizes=\"auto, (max-width: 374px) 100vw, 374px\" \/><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-1003 aligncenter\" src=\"https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_7b_WU_ACCURACY_HIST_060822_193_187.png\" alt=\"\" width=\"373\" height=\"248\" srcset=\"https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_7b_WU_ACCURACY_HIST_060822_193_187.png 576w, https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_7b_WU_ACCURACY_HIST_060822_193_187-300x200.png 300w, https:\/\/radwatch.berkeley.edu\/wp-content\/uploads\/2022\/09\/figure_7b_WU_ACCURACY_HIST_060822_193_187-272x182.png 272w\" sizes=\"auto, (max-width: 373px) 100vw, 373px\" \/><\/p>\n<p>&nbsp;<\/p>\n<p><span style=\"font-weight: 400;\">While I was unable to find any definitive correlations between the various sensor readings from WeatherUnderground and LBL\u2019s precipitation, it was made clear that the slight variations were not due to any precipitation.\u00a0<\/span><\/p>\n<p><span style=\"font-weight: 400;\">\u00a0<\/span><\/p>\n<p><br style=\"font-weight: 400;\" \/>*Featured Stock image from <a href=\"https:\/\/www.rgbstock.com\/photo\/oATae2c\/Weather+station\">RBGStock.com<\/a><\/p>\n<p><br style=\"font-weight: 400;\" \/><br style=\"font-weight: 400;\" \/><\/p>","protected":false},"excerpt":{"rendered":"<p>Introduction My work for the 2022 summer semester consisted of analyzing the accuracy of DoseNet\u2019s sensors with comparisons to nearby sensors on the WeatherUnderground network. [&hellip;]<\/p>\n","protected":false},"author":15,"featured_media":1008,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[56,18,30,17],"tags":[],"class_list":{"0":"post-986","1":"post","2":"type-post","3":"status-publish","4":"format-standard","5":"has-post-thumbnail","6":"hentry","7":"category-community","8":"category-education","9":"category-internship","10":"category-outreach","12":"post-with-thumbnail","13":"post-with-thumbnail-large"},"acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.4 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>DoseNet Summer 2022: Vikram Gill&#039;s Report - Berkeley RadWatch<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/radwatch.berkeley.edu\/es\/2022\/09\/dosenet-summer-2022-vikram-gills-report\/\" \/>\n<meta property=\"og:locale\" content=\"es_MX\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"DoseNet Summer 2022: Vikram Gill&#039;s Report - Berkeley RadWatch\" \/>\n<meta property=\"og:description\" content=\"Introduction My work for the 2022 summer semester consisted of analyzing the accuracy of DoseNet\u2019s sensors with comparisons to nearby sensors on the WeatherUnderground network. 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