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Days of average duration of insolation

Africa 10-year Average Insolation kWh/m2/day Country State/City Latitude Longitude Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year Avg BF Ouagadougou 12' 24 N 1' 30 E 5.48 6.43 6.56 6.62 6.53 6.16 5.76 5.48 5.87 6.18 5.83 5.35 6.0 In July, Oslo gets an average 17.8 hours of daylight a day. In December, it only sees sunlight for an average of 6.21 hours a day. 1 [If solar panels are tilted optimally for each month, the insolation on the panels goes up to .75 kWh/m 2 /day in December and 5.71 kWh/m 2 /day in June United States. Monthly and annual average daily insolation and temperature values have been computed from a base of 24·25 years of data, generally from 1952·1975, and I isted for each location. Insolation values represent monthly average daily totals of global radiation on a horizontal surface an average insolation intensity at the top of the atmosphere for the summer solstice at 65 N (black), the duration of the summer at 77 S (red, measured as the number of days whose diurnal average insolation exceeds 250Wm −2 ) and the number of winter days (hidden beneath the summer duration curve, measured as days below 250Wm 2 ; not

Average Daily Sunlight. The average daily sunlight (insolation) summary measure, reported in kilojoules per square meter (KJ/m 2), is the mean value of all of the daily insolation measurements that met the criteria for this cell in the results table.For example, if results are grouped by Year and limited to the South Region for years 1979-2010, then the first row shows the value 17,084.28 (KJ. To attain best results, most devices for harvesting sunlight require an insolation of greater than 3 to 4 kilowatt hours per square meter per day. Luckily, insolation is quite high year round near the equator, where roughly a billion people around the world must spend more money on fuel for cooking than they have to spend on food itself Maximum values of insolation are received at the June solstice when day length and angle of incidence are at their maximum (see Table 6h-2 and section 6h). During the June solstice day length is 18 hours and 27 minutes and the angle of the Sun reaches a maximum value of 53.5 degrees above the horizon At the top of the earth's atmosphere receives insolation is expressed as the solar constant.It received at the top of the atmospheric surface (thermopause) on a perpendicular plane to the solar beam. The average insolation received at the thermopause i.e.1368Wm2(Watt per squaremetre)energy(solar constant)in the form of short wave Solar irradiance is the power per unit area received from the Sun in the form of electromagnetic radiation as measured in the wavelength range of the measuring instrument. The solar irradiance is measured in watt per square metre (W/m 2) in SI units.Solar irradiance is often integrated over a given time period in order to report the radiant energy emitted into the surrounding environment.

The duration of insolation on March 21 is 12 hours daylight. The duration of insolation is dependent on temperature, season and latitude. On which date does the maximum duration of insolation occur.. Since insolation is a measurement over time, you will need to take the average measurement for each hour of sunlight and add these together to get the total insolation. Therefore, if you have 6 hours of sunlight, you will add 6 measurements together The amount of insolation that an area receives can vary over the course of a day or over a year. The highest point of the Sun's path in the sky is the time when the maximum amount (intensity) of insolation for the day reaches a location. The warmest part of the day is usually a few hours later Q. The diagrams below represent Earth's tilt on its axis on 4 different dates. The shaded portion represents the nighttime side of the Earth. Which diagram best represents the day on which the longest duration of insolation occurs in NY state

This visualization shows the amount of solar intensity (also called solar insolation and measured in watts per square meter) all across the globe as a function of time of day and day of year. This is an idealized calculation as it does not take into account reductions in solar intensity due to cloud cover or other things that might block the. The time is the local solar time. Set the latitude to your location and then adjust the day slider to see how much radiation there is for each day of the year. Click on the graph for numerical data. X-90 90. X. 0 80. The average daily solar insolation as a function of latitude. The three curves are the incident solar insolation,.

To get the daily average insolation, we integrate this expression between sunrise and sunset and divide by 24 hours (or 2 π radians since we express the time of day in terms of hour angle): (5) Q ¯ d a y = 1 2 π ∫ − h 0 h 0 Q d h (6) = S 0 2 π (d ¯ d) 2 ∫ − h 0 h 0 (si To aid in this calculation, the total insolation for the 15th day of each month is first calculated, and then it is assumed that this mid-month insolation remains constant during the entire month In mid-latitude continental climates, it is approximately 20-25 days in winter and 25-35 days in summer USA Global Technical & Sales Support +1 757 410-8640 1-800-916-2067 or Contact Us 9AM to 5:30 PM USA Eastern Tim

To get the daily average insolation, we integrate this expression between sunrise and sunset and divide by 24 hours (or 2 π radians since we express the time of day in terms of hour angle): Q ¯ d a y = 1 2 π ∫ − h 0 h 0 Q d h = S 0 2 π (d ¯ d) 2 ∫ − h 0 h 0 (si Figure 17. This map, similar to one from the U.S. Weather Service, shows the average annual insolation in the continental United States. The figures are in Langleys per day, not in BTU's per square foot (1 Langley = 3.69 Btu/ft2). Other maps available from the Weather Service give a monthly breakdown of insolation. Figure 17 Solar energy reaching the Earth varies with latitude, as shown above, and with the time of the year. Note that during the polar summers, the insolation is actually higher than it ever is at the equator — this is due to the increased day length; at the equator, half of the day is typically dark, with no sunlight, which brings down the daily average in comparison to the polar summer condition. duration of insolation. 4. Average annual surface temperature on the Earth are inversely related to latitude location. C. Absorption of Insolation - Approximately 19% of incoming solar radiation is absorbed by the atmosphere. 1. Approximately 47% of insolation is. 3.2. Insolation on an Inclined Plane. The inclined insolation was calculated by Lid and Jordan's equation []: where I sc is the solar constant (1367 W/m 2), n is the day number of year, is the latitude, is the solar declination, and is the sunset hour angle.The values of and can be approximately expressed by equations and (), respectively:. The daily solar insolation on an inclined plane.

time-scales. Hypothesis I - Increased insolation Months Time-Scale Taking up first the months time+&, Figs. I and 2 show the normal month-to-month poleward gradient changes of effective solar radiation absorbed by the atmosphere and the earth's surface (taking into account average albedoes) and corresponding month-to-mont On these days all over the earth the days and nights are equal. On these two days, the maximum amount of insolation is received at the equator, and the amount goes on decreasing towards the poles. But from the winter solstice (December 22) onward the length of day increases in the northern hemisphere till the summer solstice (June 21) At an angle of 30°, the insolation is only 50% as much as the maximum. Distance. The amount of energy that the Earth as a whole receives on a daily basis changes slightly during the year because of the Earth's slightly elliptical orbit. On average, the Earth is 150 million kilometers (or 93 million miles) from the Sun

The legend indicates the average (over the course of the year) amount of solar insolation (full sun hours) for these zones. These figures are based on the yearly average; consequently, systems based on these figures will provide more power in summer and less in winter. Winter figures for daily solar gain may be from 25% to 50% less than these. An insolation map can show you the amount of solar energy your location receives on an average day during the worst month of the year. Several charts and lists have compiled more specific data for North America, including monthly and seasonal averages, that you can use to determine the average number of peak sun-hours your panels are likely to. Australia Solar Hours (Insolation) Map This map illustrates the level of average daily solar radiation (insolation) measured in solar hours or sun hours which represent the average kWh/m3/day received in each area on an annual basis Estimation of net monthly insolation by considering shading factor (kWh/m^2/month) For this approximation, daily insolation is assumed to be constant throughout the month. Also, by considering average number of rainy days per month, insolation is assumed to be dropped by 50% on a rainy day There are many factors that will influence the efficiency output of solar panels in Phoenix. First, the sun and the weather. For example, peak sun hours are the amount of time in a day where the sunlight is nearest optimal levels for solar insolation, which only includes the sunlight that hits the solar panels at efficient angles with optimal strength of radiation

Day Length and Insolation - Flying Turtl

  1. To get the annual sum of radiation you have to take the annual average (kwh/m2/day) and multiply it by 365 (days). For our example (London) the annual horizontal global solar radiation is 2.79*365=1018 kWh/m2 per year. Get average monthly and annual temperature, wind, insolation and precipitation data anywhere on the globe
  2. Natural factors, such as cloud coverage, weather, time of year and much more all impact the daily sun light hours and amount of solar insolation. Not every hour of sunlight will be converted at the same efficiency ratio, so it can help to look at the average when planning for your year
  3. During a year which of the three latitudes on exercise 11 experience the least variation in average daily insolation at the top of the atmosphere and why? The equator at zero degree's because the the sun angle is all year long and constant day length all your long. How many moths of the year does the North Pole receive no insolation

24.Buenos Aires, located at 41° S, receives the shortest duration of insolation on A)0° B)23° N C)23° S D)90° N 25.On September 23, the duration of insolation at all four locations is 12 hours Tying insolation at the top of the atmo-sphere to climate on the ground poses a serious challenge. It is useful to consider empirical relationships between insolation ( 19) and mod-ern temperature ( 20). Insolation lagged by 30 days shows an excellent correlation with zonally and diurnally averaged land tempera

Daily Sunlight (Insolation) - CDC WONDE

Duration of the day varies from place to place and season to season. It decides the amount of insolation received on the earth's surface. The longer the duration of the day, the greater is the amount of insolation received. Conversely shorter the duration of the day leads to receipt of less insolation. 4. Transparency of the atmospher determine time integrated insolation at any latitude and longitude on Earth; determine sun's strength or radiation output. Read questions, answers and comments about insolation. The file SRTERMS.TXT contains the definition of terms used in calculating insolation Over a time period of 2.6 Myrs (twice the length of the previous case) the pattern of the average insolation received on Pluto is actually very similar to the pattern seen over the current single Pluto orbit, but with two key differences: (1) The difference between the average insolation received at the poles is slightly more dramatic over the. The average daily solar insolation in units of kWh/m 2 per day is sometimes referred to as peak sun hours. The term peak sun hours refers to the solar insolation which a particular location would receive if the sun were shining at its maximum value for a certain number of hours

Enter your ZIP code to find out the month-to-month and average pv insolation (DNI/Direct Standard Insolation) on your location. This pv calculator utilizes information provided by NASA and is depending on 22 years of average of collected vitality for every place At which latitude is the Sun directly overhead on certain days of the year? answer choices . 66.5° N. 90° N. 23.5° N. 42° N. Tags: Question 4 . SURVEY . 30 seconds . Report question . Q. The longest duration of insolation on December 21 will occur at. answer choices Which graph best represents the relationship between the time of day. Figure 2 shows an example of a time series plot of daily averaged insolation at a given location for one year, 2009. User's may choose start and end dates to produce time series plots and data tables that conform to their needs. Fig 1: Annual average insolation over 22 year Insolation is the amount of downward solar radiation energy incident on a plane surface. Seasonal and latitudinal variations in temperature are driven primarily by variations of insolation and average solar zenith angle. The amount of solar radiation incident on the top of the atmosphere depends on the latitude, season, and time of day

Measuring Solar Insolation - NAS

6(i). Earth-Sun Relationships and Insolatio

According to SolarInsolation.org, solar insolation is a measure of solar radiation energy received on a given surface area in a given time. It is commonly expressed as average irradiance in watts per square meter (W/m2) or kilowatt-hours per square meter per day (kW•h/(m2•day))(or hours/day) Exercise 6: How Insolation Varies with Latitude . Due to the day/night cycle, and the spherical shape of the Earth, average insolation at any location is always a fraction of the solar constant of 1367 W m-2.Given some area of surface on the planet, this fraction is the ratio of its projected area onto a circle to its actual surface area on the sphere summer insolation—glacial inception would require CO2 con-centrations below preindustrial levels of 280 ppmv (refs 2-4). However, the precise CO2 threshold4-6 as well as the timing of the hypothetical next glaciation7 remain unclear. Past in-terglacials can be used to draw analogies with the present, provided their duration is known L.O: THE ANGLE OF INSOLATION ANGLE INSOLATION: THE ANGLE SUNLIGHT HITS THE EARTH HIGHER ANGLE OF INSOLATION= MORE SUNLIGHT, LONGER DAYS, HOTTER CLIMATE A)has a lower angle of insolation B) has a higher angle of insolation C)is closer to the Prime Meridian D)is farther from the Prime Meridian 1.The graph below shows air temperatures on a clea

Solar Insolation Maps From the National Renewable Energy Labs (NREL) There are Four Maps Here: Average Yearly Sun - The first one shows the yearly average; Best Case - The 2nd one is the best case or June; Worst Case - The 3rd one is the worst case or December.; With Tracking Mount - The 4th map shows the worst case (January) again, but with a tracking panel mount, which follows the sun This is a measure of the intermittency of the solar energy source. It also means that solar systems have to be built to cope with peak intensity, but will on average only be able to convert 18% of that peak. This factor is closely related to the so-called capacity factor. Annual Variation of solar insolation The period of insolation depends on astronomical, meteorological and relief factors. Insolation is smaller in narrow valleys, river valleys and mountain ranges as a result of the increase of overcast and elevation. Kosovo has on average 2,066 hours with sun per year or approximately 5.7 hours per day

Duration Between Two Dates - Calculates number of days. Time and Date Duration - Calculate duration, with both date and time included; Date Calculator - Add or subtract days, months, years; Birthday Calculator - Find when you are 1 billion seconds old; Related Links. Date/calendar related services - Overvie These maps show where and how much sunlight fell on Earth's surface during the time period indicated. Scientists call this measure solar insolation.Knowing how much of the Sun's energy reaches the surface helps scientists understand weather and climate patterns as well as patterns of plant growth around our world Three hundred forty watts per square meter of incoming solar power is a global average; solar illumination varies in space and time. The annual amount of incoming solar energy varies considerably from tropical latitudes to polar latitudes (described on page 2). At middle and high latitudes, it also varies considerably from season to season

Insolation - Simple English Wikipedia, the free encyclopedi

To know the collect insolation of your area check the color of the country you come from and then check the value of the insolation on the scale below every map. Remember these figures are the average annual insolation. So to find the insolation on daily basis you divide the figure with 365 which is the number of days in one year Help and Example Use. Some typical uses for the Date Calculators; API Services for Developers. API for Business Date Calculators; Date Calculators. Time and Date Duration - Calculate duration, with both date and time included; Date Calculator - Add or subtract days, months, years; Weekday Calculator - What Day is this Date?; Birthday Calculator - Find when you are 1 billion seconds ol 13.The greatest duration of insolation in Jamestown occurs when the Sun appears to travel along path A)42° N B)23.5° N C)0° D)23.5° S 14.When the Sun appears to travel along path D at Jamestown, which latitude on Earth receives the mos

Based on the astronomical ephemerides DE-406, theoretical calculations have been performed of the interannual variability of the Earth's insolation related to celestial-mechanical processes for 365 points of a tropical year in the time period from 1900 to 2050. It has been determined that the average amplitude of variations of the interannual insolation is 0.310 W/m2 (0.023% of the solar. B)The duration of insolation will decrease and the temperature will increase. C)The duration of insolation will increase and the temperature will decrease. D)The duration of insolation will increase and the temperature will increase. 2.Which changes can be expected to occur at 45° N over the next 30 days? A)0° B)30° N C)60° N D)90° A historical weather API request will give you real verifiable data for any location, and time period you request. We currently have both hourly, and daily level historical data. Additionally, for users that need large volumes of data, we have a bulk historical weather API that allows for retrieval of multiple years worth of data at once Finally, it's worth considering also what happens when the solar PV panel is-as is typical-tilted. In that case, the total solar irradiation on the PV panel-in the plane of array-is the sum of three distinct components, one of which is the component which falls directly on the panel in a normal from the sun; a second component which is diffuse solar radiation from the. Hourly - K = swdsfc/swdtoa, where swdtoa is hourly average of incoming top-of-atmosphere insolation (solar constant times average cosine of the Solar Zenith Angle). Daily - sum hourly values for the day and divide by their number. Monthly - sum daily values and divide by the number of days with data

depends on the length of the day and power of maximum solar insolation [3]: P max π N E 2 =, (4) where N - duration of the day, h; Pmax - maximal power of solar insolation on the collector surface during the day, kW m-2. Duration of the day ( )ϕ δ ϖ N ≈ ≈ arccos −tg ⋅tg 15 2 15 2. (5) The maximal power of solar insolation on the. For example, you might be interested in knowing the average insolation of each panel over a period of time, or the maximum insolation of each panel at any one time At higher latitudes the length of day changes quite noticeably in early January and mid-November. In some situations two adjacent days are different in length by nearly five minutes, and at some points the day loses nearly fourty minutes over the course of a single week insolation during one year at four different latitudes on Earth's surface. 2.0 1.8 1.4 1.2 1.0 0.6 0.4 02 0.0 Insolation at Different Latitudes Equator 00 00 Jan. Feb. Mar. Apr. May Jun. Jul. Aug. Sep, Oct. Nov. Dec. Month This graph shows that insolation varies with A) latitude and time of day C) longitude and time of day hours of bright sunshine (i. e., the day length of the average day of the month), respectively. Values of can be calculated from the follow-ing equation, using recommended average days for months and values of n by months, according to (Duffie and Beckman, 1991): (2) Here GSC is the solar constant, whose value is 136

Are different. Climate is related ONLY to average precipitations over long periods of time, while weather is related ONLY to average precipitations over periods up to two weeks; 2. (3 points) How much heat (in kWh) is delivered to a 1000m2 glacier over one day with an insolation value of 6.45kWh/m2 * day? a r is the yield of the solar panel given by the ratio : electrical power (in kWp) of one solar panel divided by the area of one panel. Example : the solar panel yield of a PV module of 250 Wp with an area of 1.6 m2 is 15.6%. Be aware that this nominal ratio is given for standard test conditions (STC) : radiation=1000 W/m2, cell temperature=25 celcius degree, Wind speed=1 m/s, AM=1.5 This chart shows solar insolation in kilowatt-hours per square meter per day in many US locations. For simplicity, we call this figure Sun Hours / Day. To find the average sun hours per day in your area look at the maps at the bottom of this page, or find a city in the table below that has similar weather to your location Julian days are the ordinal number of the day of the year, starting with 1 on January 1st and ending with 365 on December 31st. The spreadsheet is designed to only accept values for latitudes and longitudes within the continental U.S. The time entry cells allow you to input the local time, time zone, and whether Daylight Saving Time is activ

Solar irradiance - Wikipedi

Climate can mean the average weather for a particular region and time period taken over 30 years. Climate is the average of weather over time. July is the hottest month for Elk Grove with an average high temperature of 92.5°, which ranks it as about average compared to other places in California Earth's temperature depends on how much sunlight the land, oceans, and atmosphere absorb, and how much heat the planet radiates back to space. This fact sheet describes the net flow of energy through different parts of the Earth system, and explains how the planetary energy budget stays in balance

What is the definition for duration of insolation? - Answer

duration of insolation, in hours, at Barrow, Alaska, on the twentieth day of each month during 2008. The map shows the location of Barrow at 71° N 156.5° W. 29. On the grid below, construct a line graph by plotting the data for the duration of insolation at Barrow for each date shown on the data table. Connect the plots with a line While the effect is evident in a daily temperature plot, it is more readily apparent by looking at changes in the monthly average temperature. In Cleveland, July averages 3.3°F degrees higher than June, with August also warmer than June by 2.8°F, even though the length of days in August is considerably less than the length of days in June Kathy, Those numbers listed correspond exactly to the solar sunlight hours as an average based on many years of data collection. Although the sun shines and gives light many more hours per day, those numbers represent the average amount of sunlight hours anybody can use to calculate how many kwh's of electricity a solar panel will produce

Solar Insolation - Understanding & Measurin

20.Buenos Aires, located at 41° S, receives the shortest duration of insolation on 21.Base your answer to the following question on the graph below which shows variations in Earth's monthly temperatures from normal Earth temperatures between January 1990 and January 1995 in apparent solar time (ie: for hour angles that are evenly divisible by 15 degs), but the value used as the denominator in each ratio was the average of the values computed for the beginning and end of the hour during which I, was measured. Similarly, the value of CC associated with each value o Given present-day insolation and average meteorology, our model predicts the Penny Ice Cap is close to equilibrium (would retreat from 800- to 900-m elevation with an equilibrium line altitude of ~1400 m), indicating that our model is appropriate for the study of the possible ice cap expansion in different climates This average is a reasonable approximation of the annual average daily energy inputs. This profile is essentially the same as the profile of average temperature by latitude. The phenomenon of high insolation at high latitudes in the summer explains how giant cabbages and such short growing season plants can be grown in Alaska

Changes in Insolation - CliffsNote

Typically expressed on an average daily basis for a given month. Also referred to as solar insolation or peak sun hours. Solar irradiation (energy) is equal to the average solar irradiance (power) multiplied by time. Peak sun hours (PSH) is the average daily amount of solar energy received on a surface. PSH are equivalent to 42 As the angle of the Sun's rays striking Earth's surface at noon changes from 90° to 43°, the length of a shadow cast by an object will (1) decrease (2) increase (3) decrease, then increase (4) increase, then decrease 43 Which graph best shows the duration of insolation at this location as the angle of insolation changes 2-14 days represents the current official estimated range for the novel coronavirus COVID-19. However, a case with an incubation period of 27 days has been reported by Hubei Province local government on Feb. 22 []; In addition, a case with an incubation period of 19 days was observed in a JAMA study of 5 cases published on Feb. 21. [An outlier of a 24 days incubation period had been for the. At year 2007 AD, Spring = about 92+ 3 / 4 days and getting shorter, Summer = about 93+ 2 / 3 days and getting longer, Autumn = about 89+ 5 / 6 days and getting longer, Winter = slightly less than 89 days and getting shorter, with an average season length in this data set of about 91 days 7h 27m 15s. The significance of the changing season. Hourly time series of modeled and measured insolation at Lincoln, NE, for (a) the month of May 2003 and (b) an enlarged look at a sequence of days 1-7 May. Lines indicate estimates from GOES-E (thin dotted) and -W (thin solid) imagery, the GOES-E/W model average (thick black), and measurements from the Lincoln USCRN station (thick gray)

Earth Science MP2 Quiz 2-02va Quiz - Quiziz

GEOG 102 Week 2 Lab: Seasonal Changes Overview Over the course of a year, the area where we live experiences seasonal changes in the amount of insolation it receives, the angle of the Sun, and the length of daylight. Seasonal changes in insolation for a location are largely driven by the angle of the Sun above the ground, and the length of daylight--both of which depend on the latitude of that. In the solar industry context the term irradiation is not used much or unambiguously. However, irradiance and insolation are extensively used and have specific meanings. Irradiance is ultimately an instantaneous value of how much energy from the s.. As the earth orbits the sun, the amount of insolation will change at any particular location, causing the seasons to change. With its elliptical orbit, the distance from the earth to the sun varies by only 5 million miles, or about 3% of the average distance from the sun (the average distance from the sun is about 150 million miles) over the. The % Sun numbers measure the percentage of time between sunrise and sunset that sunshine reaches the ground. Again, these amounts are averages based on decades of weather observations. The Total Hours figures are the average number of sunny hours that Hartford normally has each month or in a year. These totals are the averages calculated for.

Solar (Sun) Intensity By Location and Time - Engaging Dat

insolation will change at any particular location, causing the seasons to change. With its elliptical orbit, the distance from the earth to the sun varies by only 5 million miles, or about 3% of the average distance from the sun (the average distance from the sun is about 150 million miles) over the course of one year The average insolation for my total table is just over 295W/m^2, a reduced table of 10 day increments I've been using for another blog post is just under 295W/m^2. In other words, about 295W/m^2, not far off the Kiehl/Trenberth assumption of 340W/m^2 insolation [Reference 3 last line] Unfortunately, the coldest regions of the globe near the poles are areas with weaker sunshine and for, much of the year, shorter days. Insolation value -- the strength of. Any place experiencing night receives zero, whereas equatorial locations experiencing clear skies during the summer may get 600 - 700 W/m2 at noon. Something happens to the rest of the insolation between the time it reaches the atmosphere and the time it reaches the surface. 4 This means that the Sun, while not vertically overhead, is very close to vertical, and as a result we do get a great deal of insolation. In addition, our days run approximately 14 hours in length. It's warmest along 25 to 25 degrees N in the summer season because here you have both the ray (insolation) and time

The three top-of-atmosphere insolation curves in Figure 2 indicate that the most intense daily insolation d. over the period of a year occurs at the _ _ location. polar 5. Plotted on Figure 2 are data points (@) of monthly average daily top-of-atmosphere insolation at 45 degrees b. midlatitude North Latitude (45N) Angular distance between the two equinoxes is 180°, so summer (or winter) insolation matches exactly at ToA for the two hemispheres. That's astronomy so far. To absorb an equal amount of energy in a year, average all sky albedoes of the two hemispheres should also match. That's accomplished by clouds, to an astonishing degree If the insolation had been constant at 1000 W/m 2 the same amount of energy would have been received in 3.5 hours. The Equivalent Hours of Full Sun is a measure of average insolation at different locations. In this case the EHS is 3.5 hours 5) At what time of day is insolation the greatest on the surface of the Earth 6) When during the year is insolation the greatest at the North Pole? 7) Where on Earth is insolation a maximum on the Equinoxes? The tilt of Earth's spin axis is currently oriented at an angle of 23.5* relative to its orbit aroun sun

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