This document discusses climate data from Oxford, UK from various time periods. It presents temperature, rainfall, sunshine, frost and wind speed data in tables and charts. The document suggests that the way data is presented can influence judgments about climate change. It provides monthly, yearly and period climate averages from 1853 to 2009 to compare trends over time.
The document contains 6 climate graphs showing monthly temperature and rainfall data collected from different locations. The graphs show a wide range of temperatures from -27°C to 31.9°C and rainfall amounts ranging from 0 mm to 225 mm. This data suggests the locations span polar, temperate, and tropical biomes. The variety of climates represented makes it difficult to identify any single biome without additional context.
The document summarizes the typical weather conditions in Reykjavík, Iceland on April 24th, which is the Icelandic public holiday known as the First Day of Summer. It notes that on this date, the average high is 6°C/43°F, with lows of 2°C/35°F, humidity around 78%, and around 0.5mm of precipitation expected. While the climate is not truly summer-like, Icelanders still celebrate with parades and events marking the beginning of summer according to the old Norse calendar.
This document contains monthly average wind speed and direction data from 1997 and 2015 for a location at 8°N 165°E. It includes two tables displaying the average zonal (U) and meridional (V) wind components in meters per second for each month, along with yearly average values. Two line graphs show the monthly trends in zonal and meridional wind speeds for the two years.
This document provides homework questions about the causes of seasonal changes. Students are asked to copy 4 questions on which city experienced the most and least variation in temperature and daylight hours, why data fluctuated in Anchorage, why data is consistent in Quito, and to compare data between Chicago and Melbourne noting similarities and differences.
Oxford 28th october (capital costs, storage, experience curves) v2Chris Goodall
Our assumptions about the Levelised Cost of Electricity from renewables are wrong. This presentation looks at how we should correct our estimates by taking note of the fall in the real cost of capital for index-linked assets which, for example, includes PV in the UK.
This document discusses rainfall (presipitasi) in Indonesia. It defines presipitasi as water falling from the atmosphere to Earth's surface, including rain, snow, fog, dew and hail. In tropical areas like Indonesia, the main contributor is rain. Rain occurs when moist air rising in the atmosphere cools and condenses. Factors like wind, temperature, atmospheric and local pressures influence rainfall amounts. The types of rain discussed are convective (from air masses lifted by heating), cyclonic (from uneven solar heating creating pressure systems), and orographic (from moist air lifted over mountains). Methods for measuring and analyzing rainfall data using rainfall stations are also outlined.
This document summarizes hydroclimatic data from the Angelina River basin near Alto, Texas over multiple time periods. It includes stream discharge statistics from 1940-2015 that show average monthly flows ranging from 171 to 1850 cubic feet per second. USGS data from 2004-2013 includes mean annual flows, peak floods, minimum flows, and annual precipitation. The wettest year was 2007 with a peak flood of 30,000 cubic feet per second in July. The driest year was 2011 with a minimum flow of 2 cubic feet per second in September. Precipitation across four stations in the basin is also analyzed for flood and drought years to understand rainfall patterns. Daily discharge levels over 30 days of the major 2007 flood event are given.
The document contains 6 climate graphs showing monthly temperature and rainfall data collected from different locations. The graphs show a wide range of temperatures from -27°C to 31.9°C and rainfall amounts ranging from 0 mm to 225 mm. This data suggests the locations span polar, temperate, and tropical biomes. The variety of climates represented makes it difficult to identify any single biome without additional context.
The document summarizes the typical weather conditions in Reykjavík, Iceland on April 24th, which is the Icelandic public holiday known as the First Day of Summer. It notes that on this date, the average high is 6°C/43°F, with lows of 2°C/35°F, humidity around 78%, and around 0.5mm of precipitation expected. While the climate is not truly summer-like, Icelanders still celebrate with parades and events marking the beginning of summer according to the old Norse calendar.
This document contains monthly average wind speed and direction data from 1997 and 2015 for a location at 8°N 165°E. It includes two tables displaying the average zonal (U) and meridional (V) wind components in meters per second for each month, along with yearly average values. Two line graphs show the monthly trends in zonal and meridional wind speeds for the two years.
This document provides homework questions about the causes of seasonal changes. Students are asked to copy 4 questions on which city experienced the most and least variation in temperature and daylight hours, why data fluctuated in Anchorage, why data is consistent in Quito, and to compare data between Chicago and Melbourne noting similarities and differences.
Oxford 28th october (capital costs, storage, experience curves) v2Chris Goodall
Our assumptions about the Levelised Cost of Electricity from renewables are wrong. This presentation looks at how we should correct our estimates by taking note of the fall in the real cost of capital for index-linked assets which, for example, includes PV in the UK.
This document discusses rainfall (presipitasi) in Indonesia. It defines presipitasi as water falling from the atmosphere to Earth's surface, including rain, snow, fog, dew and hail. In tropical areas like Indonesia, the main contributor is rain. Rain occurs when moist air rising in the atmosphere cools and condenses. Factors like wind, temperature, atmospheric and local pressures influence rainfall amounts. The types of rain discussed are convective (from air masses lifted by heating), cyclonic (from uneven solar heating creating pressure systems), and orographic (from moist air lifted over mountains). Methods for measuring and analyzing rainfall data using rainfall stations are also outlined.
This document summarizes hydroclimatic data from the Angelina River basin near Alto, Texas over multiple time periods. It includes stream discharge statistics from 1940-2015 that show average monthly flows ranging from 171 to 1850 cubic feet per second. USGS data from 2004-2013 includes mean annual flows, peak floods, minimum flows, and annual precipitation. The wettest year was 2007 with a peak flood of 30,000 cubic feet per second in July. The driest year was 2011 with a minimum flow of 2 cubic feet per second in September. Precipitation across four stations in the basin is also analyzed for flood and drought years to understand rainfall patterns. Daily discharge levels over 30 days of the major 2007 flood event are given.
The presentation models and analyzes wind and solar energy resources for four US locations: Charlotte NC, Boston MA, Boulder CO, and Tucson AZ. Data on wind speed, solar irradiance, and other factors are used to calculate the energy output and net capacity factor for each location. Boston generally has the highest wind energy potential while Tucson has the greatest solar energy potential. Further work could involve modeling renewable energy backed by energy storage systems.
This document describes the generation of a typical meteorological solar radiation year (TMY) for Armidale, New South Wales, Australia using 23 years of daily global solar radiation data. The Finkelstein-Schafer statistical method was used to select the most representative year of data for each month based on how closely its cumulative frequency distribution matched the long-term monthly average. The resulting typical year showed monthly average radiation values ranging from a low of 10.41 MJ/m2 in June to a high of 25.88 MJ/m2 in December. Comparison of the TMY data to the long-term monthly averages showed good agreement, indicating the TMY successfully captured typical solar conditions for Armidale
This document describes the generation of a typical meteorological wind speed year (TMY) for Armidale, New South Wales, Australia using 20 years of daily wind speed data from 1994-2013. The Finkelstein-Schafer statistical method was used to select the most representative month of data from each year to compile into a single typical year. The results show wind speeds in Armidale vary throughout the year, with higher speeds in summer months and lower speeds in winter. The generated typical wind speed data will be useful for designers when sizing wind energy systems for buildings in the Armidale region.
This document describes a study that generated a Typical Meteorological Year (TMY) of wind speed data for Armidale, New South Wales, Australia. 20 years of daily wind speed data from 1994-2013 were analyzed using the Finkelstein-Schafer statistical method to select the most representative year of data for each month. The results show that wind speeds in Armidale vary throughout the year, with higher speeds in summer months and lower speeds in winter. The generated typical wind speed data can help designers size and optimize wind energy systems for the Armidale region.
This document discusses generating a realistic estimate of annual typical daily solar photovoltaic power for urban Armidale, NSW, Australia. It analyzes solar radiation data from 1990-2012 from the Armidale Airport Weather Station to create a modified test reference year that accounts for cloudy days. Equations are used to estimate yearly electricity generation potential, annual electricity production, and daily power output for a sample photovoltaic panel system. Tables show the modified test reference year solar radiation values and estimated daily power outputs, providing a more accurate representation of expected photovoltaic power generation in Armidale compared to typical meteorological data.
The document discusses the impacts of climate change based on observed data. It finds that human activities like burning fossil fuels are releasing greenhouse gases and warming the planet. This is causing glaciers and ice sheets to melt, sea levels to rise, and more extreme weather events like droughts and hurricanes. Continued emissions could have dramatic economic and environmental effects. Data shows most of the warming occurred in the last few decades and climate models match observations when human factors are included.
ICLR wildfire season forecast 2018 (Richard Carr, Canadian Forest Service)glennmcgillivray
On May 16, ICLR hosted a special webinar which provided a forecast of the 2018 wildfire season. The session was led by Richard Carr, Fire Research Analyst for the Canadian Forest Service. The interactive webinar summarized the current conditions in Canada and provided a forecast for the 2018 fire season. Richard provides fire weather processing for the Canadian Wildland Fire Information System (CWFIS) and international projects. He provides fire weather briefings to the Canadian Forest Service (CFS) fire group, the Canadian Interagency Forest Fire Centre (CIFFC), and to federal emergency response personnel, and helps provide seasonal forecasting of fire risk. He also helps provide information to the North American Seasonal Fire Assessment Outlook, and the North American Drought Monitor via AAFC’s Canadian Drought Monitor. He represents NRCan-CFS in the CIFFC Forest and Fire Meteorology Working Group.
The document contains multiple graphs and charts about unemployment in the UK economy from 1998-2013. It shows unemployment rates fluctuating between 4-8% and long-term unemployment, especially for youth, increasing after the financial crisis. Regional unemployment rates varied, with London typically lowest. Unfilled job vacancies declined from 2008-2010 but have since increased again.
ICLR Forecast: 2019 Wildfire Season (May 17, 2019)glennmcgillivray
On May 17, 2019, ICLR provided a forecast of the 2019 wildfire season led by Richard Carr from the Canadian Forest Service. The interactive webinar summarized the current conditions in Canada and provided a forecast for the 2019 wildfire season.
Richard Carr provides fire weather processing for the Canadian Wildland Fire Information System (CWFIS) and international projects. He also provides fire weather briefings to the Canadian Forest Service (CFS) fire group, the Canadian Interagency Forest Fire Centre (CIFFC), and to federal emergency response personnel, and helps provide seasonal forecasting of fire risk. Richard helps provide information to the North American Seasonal Fire Assessment Outlook, and the North American Drought Monitor via AAFC’s Canadian Drought Monitor. Richard represents NRCan-CFS in the CIFFC Forest and Fire Meteorology Working Group.
Chuan phat trien cua tre duoi 5 tuoi WHOhangntbk83
This document contains tables of standardized weight measurements for boys and girls under 5 years old according to WHO standards from 2006. The tables list ages in months along the top and left side, with columns showing the average weight as well as weights that are 1, 2, and 3 standard deviations below and above the average.
This document contains tables listing weight standards (in kilograms) for girls under 5 years old according to the WHO 2006 standards. The tables provide weight values from -3 standard deviations to +3 standard deviations in monthly intervals from birth to 60 months.
This report summarizes COVID-19 case data from Maharashtra, India as of April 5, 2020. It includes figures and tables showing trends in daily new cases, distribution of cases by age, sex, travel history, and more. Key findings are that Maharashtra has 638 total cases as of this date, with Mumbai reporting the highest at 378 cases. The mortality rate in Maharashtra is 5.04% compared to 2.42% for all of India.
The document analyzes the statistical processing of maximum daily rainfall data from the Huancabamba weather station from 1971-2009. It includes the monthly rainfall values in millimeters for each year. The purpose is to obtain rainfall values for return periods of 2, 5, 10, 25, 50, 100 and 500 years by statistically processing the data on maximum 24-hour rainfall.
The document summarizes a research project that measured and compared street level temperatures in New York City to temperatures recorded by city air quality monitors. Teams took temperature readings on sidewalks near two monitoring sites on different dates in July and August 2009. The readings were plotted against the monitor readings and analyzed using GIS software to identify street and neighborhood features that affect microclimates. Next steps discussed using the data to study how materials and urban design can help cool city temperatures.
Weekly Rainfall Analysis for Crop Planning Using Markov’s Chain Model for Kan...IJERA Editor
Weekly rainfall analysis of Kandhamal district during the period of 1965 to 2010 were taken for analysis purpose, the analysis is very much important for crop planning and analyzing the probability of occurrence of dry and wet periods. This will act as bench mark for crop planning as well as sustainable agricultural management of Kandhamal district which comes under the agro-climatic zone of East-coast hill region. Markov chain model has been utilized to derive the probability of dry or wet weeks and also forward and backward accumulation of rain water suitable for crop production. This analysis can be helpful to find out different cropping system including intercropping and sequence cropping suitable during that period.
The effects of weather on construction scheduling webinar
Monday 22 October 2018
Speaker:
Dr Pablo Ballesteros-Pérez and Dr Stefán Thor Smith
The link to the write up page and resources of this webinar:
https://www.apm.org.uk/news/the-effects-of-weather-on-construction-scheduling-webinar/
You can easily change/correct a name on your flight ticket under the American Airlines name change policy. The airline provides multiple online and offline modes to place a name change request. To learn more about how to change a name on American Airlines ticket, you can directly approach the airline’s customer support. Moreover, you can connect with a flight expert at +1-866-738-0741 for quick assistance.
Assessing the Influence of Transportation on the Tourism Industry in Nigeriagsochially
This research dissertation investigates the complex interplay between transportation and the tourism industry in Nigeria, aiming to unravel critical insights that contribute to the enhancement of the overall tourist experience. The study employs a multi-faceted approach, literature review establishes a robust theoretical framework, incorporating The Service Quality and Satisfaction Theory to guide the research questions and hypotheses.
The methodology involves the distribution of a structured questionnaire, ensuring a representative sample and facilitating a comprehensive analysis of the gathered data.
Key findings include the nuanced perceptions of transportation infrastructure adequacy, safety and security concerns, financial influences on travel decisions, and the cultural and ecological impacts of transportation choices. These findings culminate in a comprehensive set of recommendations for policymakers and practitioners in the Nigerian tourism industry. The findings contribute to the existing literature by providing actionable insights for policymakers, stakeholders, and researchers in the Nigerian tourism sector.
The recommendations encompass gender-sensitive planning, infrastructure enhancements, safety measures, and strategic interventions to address financial constraints, ensuring a holistic and sustainable development of the tourism industry in Nigeria.
Author: Imafidon Osademwingie Martins
The presentation models and analyzes wind and solar energy resources for four US locations: Charlotte NC, Boston MA, Boulder CO, and Tucson AZ. Data on wind speed, solar irradiance, and other factors are used to calculate the energy output and net capacity factor for each location. Boston generally has the highest wind energy potential while Tucson has the greatest solar energy potential. Further work could involve modeling renewable energy backed by energy storage systems.
This document describes the generation of a typical meteorological solar radiation year (TMY) for Armidale, New South Wales, Australia using 23 years of daily global solar radiation data. The Finkelstein-Schafer statistical method was used to select the most representative year of data for each month based on how closely its cumulative frequency distribution matched the long-term monthly average. The resulting typical year showed monthly average radiation values ranging from a low of 10.41 MJ/m2 in June to a high of 25.88 MJ/m2 in December. Comparison of the TMY data to the long-term monthly averages showed good agreement, indicating the TMY successfully captured typical solar conditions for Armidale
This document describes the generation of a typical meteorological wind speed year (TMY) for Armidale, New South Wales, Australia using 20 years of daily wind speed data from 1994-2013. The Finkelstein-Schafer statistical method was used to select the most representative month of data from each year to compile into a single typical year. The results show wind speeds in Armidale vary throughout the year, with higher speeds in summer months and lower speeds in winter. The generated typical wind speed data will be useful for designers when sizing wind energy systems for buildings in the Armidale region.
This document describes a study that generated a Typical Meteorological Year (TMY) of wind speed data for Armidale, New South Wales, Australia. 20 years of daily wind speed data from 1994-2013 were analyzed using the Finkelstein-Schafer statistical method to select the most representative year of data for each month. The results show that wind speeds in Armidale vary throughout the year, with higher speeds in summer months and lower speeds in winter. The generated typical wind speed data can help designers size and optimize wind energy systems for the Armidale region.
This document discusses generating a realistic estimate of annual typical daily solar photovoltaic power for urban Armidale, NSW, Australia. It analyzes solar radiation data from 1990-2012 from the Armidale Airport Weather Station to create a modified test reference year that accounts for cloudy days. Equations are used to estimate yearly electricity generation potential, annual electricity production, and daily power output for a sample photovoltaic panel system. Tables show the modified test reference year solar radiation values and estimated daily power outputs, providing a more accurate representation of expected photovoltaic power generation in Armidale compared to typical meteorological data.
The document discusses the impacts of climate change based on observed data. It finds that human activities like burning fossil fuels are releasing greenhouse gases and warming the planet. This is causing glaciers and ice sheets to melt, sea levels to rise, and more extreme weather events like droughts and hurricanes. Continued emissions could have dramatic economic and environmental effects. Data shows most of the warming occurred in the last few decades and climate models match observations when human factors are included.
ICLR wildfire season forecast 2018 (Richard Carr, Canadian Forest Service)glennmcgillivray
On May 16, ICLR hosted a special webinar which provided a forecast of the 2018 wildfire season. The session was led by Richard Carr, Fire Research Analyst for the Canadian Forest Service. The interactive webinar summarized the current conditions in Canada and provided a forecast for the 2018 fire season. Richard provides fire weather processing for the Canadian Wildland Fire Information System (CWFIS) and international projects. He provides fire weather briefings to the Canadian Forest Service (CFS) fire group, the Canadian Interagency Forest Fire Centre (CIFFC), and to federal emergency response personnel, and helps provide seasonal forecasting of fire risk. He also helps provide information to the North American Seasonal Fire Assessment Outlook, and the North American Drought Monitor via AAFC’s Canadian Drought Monitor. He represents NRCan-CFS in the CIFFC Forest and Fire Meteorology Working Group.
The document contains multiple graphs and charts about unemployment in the UK economy from 1998-2013. It shows unemployment rates fluctuating between 4-8% and long-term unemployment, especially for youth, increasing after the financial crisis. Regional unemployment rates varied, with London typically lowest. Unfilled job vacancies declined from 2008-2010 but have since increased again.
ICLR Forecast: 2019 Wildfire Season (May 17, 2019)glennmcgillivray
On May 17, 2019, ICLR provided a forecast of the 2019 wildfire season led by Richard Carr from the Canadian Forest Service. The interactive webinar summarized the current conditions in Canada and provided a forecast for the 2019 wildfire season.
Richard Carr provides fire weather processing for the Canadian Wildland Fire Information System (CWFIS) and international projects. He also provides fire weather briefings to the Canadian Forest Service (CFS) fire group, the Canadian Interagency Forest Fire Centre (CIFFC), and to federal emergency response personnel, and helps provide seasonal forecasting of fire risk. Richard helps provide information to the North American Seasonal Fire Assessment Outlook, and the North American Drought Monitor via AAFC’s Canadian Drought Monitor. Richard represents NRCan-CFS in the CIFFC Forest and Fire Meteorology Working Group.
Chuan phat trien cua tre duoi 5 tuoi WHOhangntbk83
This document contains tables of standardized weight measurements for boys and girls under 5 years old according to WHO standards from 2006. The tables list ages in months along the top and left side, with columns showing the average weight as well as weights that are 1, 2, and 3 standard deviations below and above the average.
This document contains tables listing weight standards (in kilograms) for girls under 5 years old according to the WHO 2006 standards. The tables provide weight values from -3 standard deviations to +3 standard deviations in monthly intervals from birth to 60 months.
This report summarizes COVID-19 case data from Maharashtra, India as of April 5, 2020. It includes figures and tables showing trends in daily new cases, distribution of cases by age, sex, travel history, and more. Key findings are that Maharashtra has 638 total cases as of this date, with Mumbai reporting the highest at 378 cases. The mortality rate in Maharashtra is 5.04% compared to 2.42% for all of India.
The document analyzes the statistical processing of maximum daily rainfall data from the Huancabamba weather station from 1971-2009. It includes the monthly rainfall values in millimeters for each year. The purpose is to obtain rainfall values for return periods of 2, 5, 10, 25, 50, 100 and 500 years by statistically processing the data on maximum 24-hour rainfall.
The document summarizes a research project that measured and compared street level temperatures in New York City to temperatures recorded by city air quality monitors. Teams took temperature readings on sidewalks near two monitoring sites on different dates in July and August 2009. The readings were plotted against the monitor readings and analyzed using GIS software to identify street and neighborhood features that affect microclimates. Next steps discussed using the data to study how materials and urban design can help cool city temperatures.
Weekly Rainfall Analysis for Crop Planning Using Markov’s Chain Model for Kan...IJERA Editor
Weekly rainfall analysis of Kandhamal district during the period of 1965 to 2010 were taken for analysis purpose, the analysis is very much important for crop planning and analyzing the probability of occurrence of dry and wet periods. This will act as bench mark for crop planning as well as sustainable agricultural management of Kandhamal district which comes under the agro-climatic zone of East-coast hill region. Markov chain model has been utilized to derive the probability of dry or wet weeks and also forward and backward accumulation of rain water suitable for crop production. This analysis can be helpful to find out different cropping system including intercropping and sequence cropping suitable during that period.
The effects of weather on construction scheduling webinar
Monday 22 October 2018
Speaker:
Dr Pablo Ballesteros-Pérez and Dr Stefán Thor Smith
The link to the write up page and resources of this webinar:
https://www.apm.org.uk/news/the-effects-of-weather-on-construction-scheduling-webinar/
You can easily change/correct a name on your flight ticket under the American Airlines name change policy. The airline provides multiple online and offline modes to place a name change request. To learn more about how to change a name on American Airlines ticket, you can directly approach the airline’s customer support. Moreover, you can connect with a flight expert at +1-866-738-0741 for quick assistance.
Assessing the Influence of Transportation on the Tourism Industry in Nigeriagsochially
This research dissertation investigates the complex interplay between transportation and the tourism industry in Nigeria, aiming to unravel critical insights that contribute to the enhancement of the overall tourist experience. The study employs a multi-faceted approach, literature review establishes a robust theoretical framework, incorporating The Service Quality and Satisfaction Theory to guide the research questions and hypotheses.
The methodology involves the distribution of a structured questionnaire, ensuring a representative sample and facilitating a comprehensive analysis of the gathered data.
Key findings include the nuanced perceptions of transportation infrastructure adequacy, safety and security concerns, financial influences on travel decisions, and the cultural and ecological impacts of transportation choices. These findings culminate in a comprehensive set of recommendations for policymakers and practitioners in the Nigerian tourism industry. The findings contribute to the existing literature by providing actionable insights for policymakers, stakeholders, and researchers in the Nigerian tourism sector.
The recommendations encompass gender-sensitive planning, infrastructure enhancements, safety measures, and strategic interventions to address financial constraints, ensuring a holistic and sustainable development of the tourism industry in Nigeria.
Author: Imafidon Osademwingie Martins
Un viaje a Buenos Aires y sus alrededoresJudy Hochberg
A travelogue of my recent trip to Argentina, most to Buenos Aires, but including excursion to Iguazú waterfalls, Tigre, and Colonia del Sacramento in Uruguay
How do I plan a Kilimanjaro Climb?
Planning to climb Mount Kilimanjaro is an exciting yet detailed process. Here’s a step-by-step guide to help you prepare for this incredible adventure.
What Challenges Await Beginners in SnowshoeingSnowshoe Tahoe
Discover the exhilarating world of snowshoeing through our presentation, highlighting the challenges faced by beginners. From physical exertion to technical finesse and braving harsh winter conditions, each step in the snow brings new obstacles and unforgettable adventures. Embrace the challenge and conquer the winter wonderland with confidence!
Discovering Egypt A Step-by-Step Guide to Planning Your Trip.pptImperial Egypt
Travelling to Egypt is like stepping into a time capsule where the past and present coexist, offering a unique blend of history, culture, and stunning landscapes.
See more: https://imperialegypt.com/tour-packages/
How To Change Your Name On American Airlines Aadvantage.pptxedqour001namechange
American Airlines permits passengers to change/correct names on their AAdvantage account. Also, you can request a name change both online via a web portal and offline over the phone. For further information on how to change your name on American Airlines Advantage, get in touch with the airline’s customer service. Also, you can reach out to a consolidation desk at +1-866-738-0741 for quick assistance.
Best Places to Stay in New Brunswick, Canada.Mahogany Manor
New Brunswick, a picturesque province in eastern Canada, offers a plethora of unique and charming places to stay for every kind of traveler. From the historic allure of Fredericton and the vibrant culture of Saint John to the natural beauty of Fundy National Park and the serene coastal towns like St. Andrews by-the-Sea, there's something for everyone. Whether you prefer luxury resorts, cozy inns, rustic lodges, or budget-friendly options, the best places to stay in New Brunswick ensure a memorable stay, allowing you to fully immerse yourself in the province's rich history, stunning landscapes, and warm hospitality.
https://www.mmanor.ca/blog/best-5-bed-and-breakfast-new-brunswick-canada
Our excursions in tahiti offer stunning lagoon tours, vibrant marine life encounters, and cultural experiences. We ensure unforgettable adventures amidst breathtaking landscapes and serene waters. For more information, mail us at tracey@uniquetahiti.com.
Wayanad-The-Touristry-Heaven to the tour.pptxcosmo-soil
Wayanad, nestled in Kerala's Western Ghats, is a lush paradise renowned for its scenic landscapes, rich biodiversity, and cultural heritage. From trekking Chembra Peak to exploring ancient Edakkal Caves, Wayanad offers thrilling adventures and serene experiences. Its vibrant economy, driven by agriculture and tourism, highlights a harmonious blend of nature, tradition, and modernity.
22. Average daily January minimum temperature What did this chart look like five years ago? Source: Met Office
23. 2010 * Average daily January minimum temperature And what about this year? Source: Met Office
24. 1961-1990 1971-2000 2009 Average daily maximum (degrees Celsius) Average daily minimum (degrees Celsius) 13.8 14.1 15.2 6.4 6.7 7.0 Summary Oxford data Source: Met Office
Editor's Notes
This presentation consists of 23 slides looking at climate data from the Oxford temperature recording station. This station has been recording continuously from 1853, although much older data from Oxford contributes to the 'Central England Temperature Record' which is said to be the oldest temperature series in the world. The data from Oxford was originally collected at the Radcliffe (astronomical) Observatory somewhat to the north of the original city boundary. Myles Allen, the Oxford climate scientist, tells me that originally the temperature data was collected in the upper room at the Observatory 'with the windows open'. I guess –and it is only a guess - that the 1853 record starts at the point that the thermometer moved outside. Myles said that he thought the collector moved to the airfield at Benson – about 20km from Oxford – in the 1940s. Benson will have slightly different readings and the temperature series will have had to be normalised to adjust for this. This is exactly the problem with temperature readings like this: we can never get a perfect and unimpeachable data set. My purpose in assembling the following slides is to show how the climate record can be used to show very different trends, depending on the data being looked at and the slant the observer places on the numbers. Let's look first at the Metrological Office ('Met Office' for UK readers) summary of recent climate in Oxford. The figures on slide 1 are for the thirty year period from 1971-2000. Every ten years, the Met Office produces an average and updates this series. The 1971-2000 record shows the monthly average daily highs and the average daily lows. It also has the number of airfrost days, the monthly average rainfall and the typical number of days on which more than 1mm of rain fell. The wind data isn’t recorded for the city.
This sheet is from the Met Office web site and gives the thirty year averages for monthly average daily maxima and minima as well as information on airfrost, sunshine and rainfall.
The Met Office also publishes the full record of data for most of this information back to 1853. You can find it on the Met Office web site. Slide 2 shows how the raw data looks on the page. There's information about monthly average daily highs and lows, airfrost days ('af') and some rainfall data. Anybody can put this data into a spreadsheet and look at averages and trends.
In Slide 3, I plot the monthly maximum temperature for three periods: 1961-1990, 1971-2000 and for 2009. (By the way the Met Office uses 30 year averages partly because some climate drivers, such as changes in the output of the sun, swing around in about thirty year cycles). You can see that the maximum temperature has risen in later periods. Of course one year's records don’t mean anything much, but 2009 was generally higher than the later thirty year period. 1971-2000 was hotter than 1961-1990. This probably surprises you – 2009 wasn’t thought to be a warm year and the summer rainfall was quite high in Oxford. More than anything else this tends to show that we don’t have a good sense of whether today's temperatures are higher or lower than average. We – quite literally – acclimatise.
Approximately the same pattern is seen for January minima. But in 2009, the winter was much colder than in the two thirty year periods.
In Slide 5 I present this data in a more sensible form – as yearly averages. This shows that the 1961-1990 averages are about 0.3 degrees below the 1971-2000 figures.
I'm now going to look at the longer term record to see what we can say about changes in Oxford's climate. Slide 6 examines the record for the number of months with over 100mm rainfall. You can see that in most years there are a small number of months with rainfall over this level.
When we get data like this it isn’t visually obvious whether the trend is increasing or decreasing, or indeed whether there is any trend at all. We have two techniques we can use: averaging the data over a period of years and plotting a trend line on the chart. Slide 8 looks first at a ten year moving average. The number we plot is the simple mean of a year and the nine previous years. So the 1910 10 year moving average is the mean of the ten years 1901 to 1910. This slide gives us much more information – we can see that the occurrence of high monthly rainfall appears to go in cycles and the trend is generally upwards.
When we plot a trend line (simple linear regression for fans of these things), it becomes clear that the statistical trend is indeed rising. In the middle of the 19th century, we would have expected about 0.8 months of high rainfall compared to about 1.2 now. But it is very important to note that the cycles around the trend line mean that at three periods in the past the ten year average was well above the what we might predict today for the very long term average. Around 1920, the figure was about 1.5 months a year, for example. What's clear about this chart and many of those that follow is that there is a lot of 'noise' in climate data compared to the relatively slow pace of change in the underlying 'signal'. By the way, climate scientists generally expect the intensity of rainfall events to rise as a result of the greater energy levels in the atmosphere. So the trend may continue and – as a result – Oxford's river flooding problems are possibly going to get more severe
If we plot a moving average over a longer period – the thirty year cycle I mentioned earlier - the pattern looks very different. A quick scan suggests that the frequency of high rainfall months hasn’t increased much at all. The lesson is clear: how we present the data really does affect the impression we give our readers.
In slide 10, I put the trend line back. Unsurprisingly to those of you with a little mathematics, the trend is almost the same as with the 10 year moving average.
In Slide 11, I move to look at the number of airfrost days. (An airfrost day in one on which the temperature ever drops below zero at, I think, one metre above ground level.) The ten year moving average shows a fairly steady fall, consistent with the theory that the climate is getting warmer.
In this case, if we plot a 30 year moving average, the chart becomes much clearer to the casual viewer. The decline looks impressively regular and predictable.
In the next slide, we can see a much less regular picture. If you just plot the number of airfrost days in April – the end of the frost season in our part of the world – you see a line that drops sharply until 1970 and then rises quite quickly. If you wanted to question whether climate change was actually happening in Oxford you might say that the evidence suggests that the frost season is no shorter now than it was in 1970. This wouldn’t really be a fair statement – after all the trend line is strongly downward – but you would be literally correct in what you said.
Let's move on to temperatures. Here's the ten year moving average for daily maximum July temperatures. Once again, a quick look says that the warmth of the 1870's matches today's figures and, moreover, in recent years July maxima have actually fallen from the peak of the early 2000s.
Putting a trend line on the graph shows a more balanced picture. Over the last 150 years, the statistical tendency has been upward, although the change isn’t great.
The next chart shows the twenty year average and the pattern appears clearer and the 1870s peak isn’t higher than recent figures.
The thirty average produces a strikingly more convincing chart
January minima have tended to rise. But plotted as a ten year average, the pattern isn’t at all clear.
It becomes easier to see with a twenty year average and with a trend line added for visual clarity.
But the thirty year pictured without a plotted trend gives a strong visual sense that the trailing average in 1930 was about the same as the 1990s.
And if you present the data without the last five or so years the effect is to suggest a cycle that isnt showing much rise, even when you plot the trend as well.
And if you include the 2010 figure, the effect is quite striking to the eye.
What I've tried to show that climate data is so variable and 'noisy' that trends are difficult to determine, even at one single recording station. This means two things. Anybody wanting to put their own spin on the data is quite able to do so. And, second, that any reasonably sceptical person can legitimately note the predictably unpredictable outcomes and say that the underlying trends are really quite unclear. But the fact is that Oxford is, on long-term averages, getting a little bit warmer and more rainstormy each year. I think the rational person looks at the record and says that weather variability is very high but the trends are fairly obvious. The climate scientists tell us that the world climate has a great deal of momentum. With the heat trapping gases already in the atmosphere, we are likely to see continued warming even if we stop burning fossil fuels tomorrow. In Oxford, the main implication is that the Thames is probably going to flood more often. If you are affected by this, it is utterly devastating. But we can cope with temperatures quite a lot hotter than today with few ill effects. In other parts of the world, already on the margins of human survival, continued human habitation is at threat as rivers dry up and summer temperatures reduce agricultural production.