what to do before, during and after volcanic eruption pptFor most years starting in the 1990s, the extent of ozone Since the 1960s, ground-based and satellite instruments have recorded variations in the total energy emitted by the Sun, which is well correlated with changes in solar UV radiation. Peak depletion occurs in early October when ozone is often completely destroyed over a range of stratospheric altitudes, thereby reducing total ozone by as much as two-thirds at some locations. If a decline in solar output were the primary cause of the long-term decline in global total ozone, then the solar output would exhibit a similar long-term decrease. The influence of these tropospheric systems extended poleward and upward into the stratosphere, disturbing the normal circumpolar wind (polar vortex) and warming the lower stratosphere where ozone depletion was ongoing. With increased ClO, the catalytic cycles involving ClO and BrO become active in the chemical destruction of ozone whenever sunlight is available (see Q8). extensively explored with specialized computer models (see Q20). Low-GWP substances. is produced naturally in the stratosphere by a two-step At geographic locations with the lowest total ozone values, balloon measurements show that the chemical destruction of ozone has often been complete over an altitude region of up to several kilometers. ozone destruction because Cl and ClO Since 1997, total ozone has increased in the range of 0.3-1.2% employing this information were used to simulate how This week in maths I am asking that children complete the activities on the website above. Adding up the source gases with the reactive gases Use your topic book to turn the negative comments into positives and write your own negative comments that you need to turn to positives. output for October, since this is the month of peak ozone depletion in the Antarctic region (see Figure Q10-3). However, Arctic ozone depletion is less severe than that observed in the Antarctic and exhibits larger year-to-year differences as a consequence of the highly variable meteorological conditions found in the Arctic polar stratosphere. Figure Q1-3. Halogen source gases containing chlorine and bromine controlled under the Montreal Protocol are referred to as ozone-depleting substances (ODSs). Reactive chlorine in polar regions. Depletion of the ozone layer increases primarily If volcanic activity were the primary cause of the long-term ozone decline, then stratospheric The variations are demonstrated here with two-week averages Everyday, there is a series of lessons in different subjects displayed on the link above and children can click the lesson they want to complete. For all of the emission scenarios shown in Figure Q18-1, the annual emissions of each gas are added together after being weighted (multiplied) by their corresponding Ozone Depletion Potential (ODP) (upper left) or Global Warming Potential (GWP) (upper right) (see Q17 and Table Q6-1). After 1982, Since 2010, global ozone The following link provides videos of the different strategies used should children require assistance. By the end of the century, increased abundances of N2O deplete more ozone than ODSs for the scenario used here (RCP 6.0). Alterations in precipitation amounts and patterns may also occur. averages of springtime total ozone climate benefit can be realized if the energy efficiency performance of new and replacement refrigeration and air conditioning Additional causes of UV changes. Stratospheric ozone production. international scientific assessments of ozone depletion that have been produced periodically since 1989 under the auspices of reach large values. severe ozone depletion occurs each winter of surface UV radiation that is harmful to humans Another warming event in 1988 caused somewhat smaller changes in the ozone hole features than in 2002. the Arctic spring. Estimates of long-term changes in the atmospheric abundances of ODSs are based upon: (1) their measured abundances in air trapped for years within accumulated snow in polar regions, (2) observed atmospheric abundances using ground-based measurements, (3) projections of future abundances based on estimated future demand and compliance with Montreal Protocol provisions for the production and consumption of ODSs, and (4) emissions from ODS banks. between 1979 and 2008, a time of global ozone Human activities are the largest source of chlorine reaching During the total time of its stay in the stratosphere, a chlorine atom can thus destroy many thousands of ozone molecules. Observations of the ozone layer showed that depletion was indeed The since the early 1970s. The large uncertainty in the climate forcing due to release of air pollutants reflects our limited knowledge of changes in the abundance of tropospheric ozone between 1750 and the mid-1950s as well as the difficulty in modeling the complex chemical processes that control the production of tropospheric ozone. (A megatonne = 1 million (106) metric tons = 1 billion (109) kilograms. Ozone depletion and global climate change are linked because both ozone-depleting substances and their substitutes are greenhouse gases. These research findings are explained in more detail in the box below. Today's task is for children to be an estate agent and try and persuade me why i should buy a house near recently erupted volcano. Natural variations. Most of the material is an update to that presented in previous Please get in touch via the email address email@example.com if you need anything. Ozone was discovered in laboratory experiments in the mid-1800s. Children are to locate the New 7 Wonders (list attached) of the World on their map. Think about things you are thankful for and add these to the bubbles. The Montreal Protocol, strengthened by its Amendments and Adjustments, has successfully controlled the production In the tropics, the change in total ozone through the progression of the seasons is much smaller than in the polar regions. Spring Arctic and Antarctic balloon-borne measurements are shown in Figure Q11-3. Excessive exposure to UV-B radiation increases the risks of skin cancer, cataracts, We fully understand that working with your children while, in many cases, trying to work yourselves is difficult. High ClO abundances generally cause ozone depletion to continue in the Antarctic region until mid-October (spring), when the lowest ozone values usually are observed (see Q10). The upper limits of annual reductions in ODP-weighted emissions are derived from the world-avoided scenario. seen with the human eye when the Sun is near the horizon. The gases with smaller values of ODP generally have shorter atmospheric lifetimes or contain fewer chlorine and bromine atoms. The term âozone holeâ came about as a description of the very low values In the last decades of this century, this balance results in ozone levels that are just above 1960 values. used to assess past ozone changes With satellite observations, the UV-B radiation changes can be separately attributed to changes in ozone and clouds (see Figure Q16-1). ozone minimum was observed half a decade before the EESC maximum was reached. The This region has come to be called the âozone holeâ because of the near-circular contours of low ozone values in the maps. This situation leads to more meteorological disturbances in the Northern Hemisphere, which increase the mixing in of air from lower latitudes that warms the Arctic stratosphere. to UV-B radiation is a principal objective of the Montreal Protocol. within the ozone layer. The reductions in GWP-weighted emissions since the 1987 peak represent lower limits of the annual emissions avoided by the Montreal Protocol, which are a measure of its climate protection from human activities. provisions of the Montreal Protocol is required to ensure that EESC will continue to decrease as projected (see Q14). Over the past few years, observed global ozone has been about 2.2% lower than the 1964â1980 average. The surface abundances of individual gases shown here were obtained using a chemistry that augment the increase in ozone As a result of these large-scale transport and mixing processes, the ozone hole typically disappears by mid-December. Ozone in the stratosphere (Good ozone). With its slow decline, EESC will remain above the 1960 value throughout this century. Future compliance with the Montreal Protocol. (see Figure Q12-1). Children may have done some research about a volcano that erupted in Iceland recently. chlorine (EESC) for the midlatitude, Thereafter, this percentage has steadily decreased and was 2â3% of global CO2 emissions in 2018. Also, while Earthâs surface is expected to continue to warm in response to positive radiative forcing (RF) of climate from GHGs (see Q17), the stratosphere is expected to continue to cool. Figure Q20-3. At times of relatively low EESC, such as the early 1960s, total ozone is not as sensitive to a volcanically induced increase in stratospheric aerosol as during current times, when values of EESC are much higher than background levels. for reference in the upper panel. Ozone depletion by halogen source gases occurs globally (see Q12). The severe depletion of stratospheric ozone in late winter and early spring in the Antarctic is known as the âozone holeâ (see Q10). The emissions, when weighted by their potential to destroy ozone, peaked in the Both measures of ozone show substantial depletion since 1980. If you follow the link this will take you to the login page. Individual ODS reductions. Ozone in the atmosphere. The magnitude of Antarctic ozone depletion gradually increased beginning in 1980. of stratospheric sulfate particles, and Afternoon learning-week beginning 22nd June. Improvements in the energy efficiency of equipment in this sector during the transition to low-GWP alternative refrigerants could potentially double the direct climate benefits of the Amendment. The I hope you are all well and I am looking forward to seeing you next week for your transition session in school. Events represent the occurrence of important scientific findings, the completion of international scientific assessments, Source gas molecules that are not converted are transported to the stratosphere. Geophysical Year. They concluded that changes in atmospheric ozone over the 1750-2011 time period caused solely by the release of ODSs led to a cooling of –0.18 W/m2 with a range of uncertainty spanning –0.03 to –0.33 W/m2 and that changes in atmospheric ozone over the same time period caused only by release of air pollutants led to a warming of +0.50 W/m2 with a range of uncertainty spanning +0.30 to +0.70 W/m2. Ozone depletion is also observed at midlatitudes. How Do We Keep Children Safe At St Michael's? sought a better understanding of this threat to the ozone layer. The initial step in the depletion of stratospheric ozone by human activities is the emission, at Earthâs surface, of gases that contain chlorine and bromine and have long atmospheric lifetimes. The accompanying worksheets are below alongside the answers. Similar volcanic eruptions, especially until the middle of this century while EESC values are high, are also expected to reduce total ozone for a few years. have been removed from the observational data set. In case we need more time to master your paper, we may contact you regarding the deadline extension. Similar to the Antarctic (see Q10), Arctic ozone depletion occurs because of (1) periods of very low temperatures, which lead to the formation of polar stratospheric clouds (PSCs); (2) the large abundance of reactive halogen gases produced in reactions on PSCs; and (3) the isolation of polar stratospheric air, which allows time for chemical destruction processes to occur. Other instruments measure ozone remotely over long distances by using ozoneâs unique optical absorption or emission properties. due to stratospheric winds at the boundary of the polar vortex. 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