Education in india and Women Empowermentkunalgate125
This the outcome of my 6 months of research on the state of Education in India with an emphasis on Education of girl child and women and discusses related issues and roadmap for further educational reform focusing on quality and not just quantity.
Any comments and suggestions are welcome..!
Education in india and Women Empowermentkunalgate125
This the outcome of my 6 months of research on the state of Education in India with an emphasis on Education of girl child and women and discusses related issues and roadmap for further educational reform focusing on quality and not just quantity.
Any comments and suggestions are welcome..!
Satellite passive microwave measurements of the climate crisisChelle Gentemann
Invited presentation at the NASEM Committee on Radio Frequencies 2021 Fall Meeting. An overview of how passive microwave measurements are used to understand climate change.
A recent cold spell hits Puget Sound lowlands, interrupting this year’s warmer air temperatures. The warm ocean coincides with new maximum water temperatures observed throughout Puget Sound in October! Hood Canal’s higher dissolved oxygen and cold water anomalies are disappearing. November brings cold water from Whidbey Basin into Puget Sound with moderate levels of chlorophyll fluorescence. Abundant smacks of jellyfish in finger inlets of South Sound observed from our flight. Red-brown blooms remain strong in smaller bays of South Sound. Visible suspended sediments in the coastal estuaries from rain, wind, and waves. Playing in the water? Visit our BEACH program.
Lower than expected air temperatures and sunshine are now both increasing; rivers are generally running high. Willapa Bay unfolds its beauty from a bird’s-eye view. The spring phytoplankton bloom is picking up in Puget Sound. A large red-orange-brown bloom persists in southern Hood Canal at a scale sufficient for the MODIS satellite to pick up. Jellyfish are still going strong in southern inlets. Ocean climate indices (PDO, NPGO and Upwelling Index) explain much of the variability in Puget Sound temperature, salt and oxygen. Nutrients, however, are steadily increasing while sub-surface algal pigments (chlorophyll a) are declining!
After weeks of clouds and warmer air, blue skies and cold temperatures set in. Strong tidal fronts and sediment-rich brackish plumes leave Whidbey Basin and move into Admiralty Reach. A pod of Orcas follows the edge of the plume heading north! Red-brown blooms continue in Henderson, Eld, and northern Budd Inlets. Long organic debris lines are numerous in northern Budd Inlet, Hood Canal, and in Central Sound north of Edmonds (Triple Junction). Conditions in the water column in Puget Sound continue to normalize after seven months of lower oxygen. Water is very clear for this time of the year, particularly in the north.
Impact of Sea Level Rise from Storm Surge USADag Lohmann
We're quantifying the impact that a 30cm sea level rise has on losses from hurricanes for each individual location in the USA. We're also looking at losses from a hypothetical sea level in the year 1900. Summaries are shown by state and selected maps.
Summary of results: Based on current conditions of exposure (e.g. buildings and other economic assets) we have an annual average loss of about $5 Billion from our simulations. Given the sea level in 1900 that loss would go to $4 Billion. Current projections of sea level rise vary widely, but most have us exceed 30cm between 2040 and 2080. Some go much higher (many meters), while the most optimistic ones are around 30cm at the end of the century. Given the same exposure, same sea defenses, and same hurricanes, losses would go up to an average of $6.9 Billion / year (called the average annual loss or AAL).
The pattern of colder and fresher Puget Sound water persists. Jellyfish aggregations continue to persist in Budd Inlet. Debris lines are numerous and long. There are multiple oil sheens in Seattle waterways. CDOM (colored dissolved organic matter) sensor and en route ferry thermosalinograph provide an important tracer for freshwater entering Puget Sound from Whidbey Basin.
Click on Figure 2B-1 to open it in a new browser tab. This works f.pdfbaraeaaa
Click on Figure 2B-1 to open it in a new browser tab. This works for all figures. 1. Frost occurs
if the temperature falls to 32F or lower, so the date of the last spring frost in 2020 at Grand
Island was near May. a. 1 b. 10 c. 22 d. 28 2. The date of the year's first fall frost was on or
around October. a. 1 b. 13 c. 20 d. 29
Figure 2B-2. Grand Island meteorological data for 2020. 3. had the lowest average temperature
(average dry bulb), which was F. a. December 32.3 b. January ... 27.4 c. February 31.9 4. In ,
Grand Isle saw its highest average temperature at F. a. June ...77.6 b. July ... 77.4 c. August ...
79.9 5. How many days in the year had temperatures of 90F or higher? a. 21 b. 23 c. 37 d. 50 6.
How many days had temperatures of 0F or lower? a. 2 b. 17 c. 24 d. 33
7. In 2020 , Grand Island experienced about times more heating degree days than cooling degree
days. a. 2 b. 4 c. 8 d. 10 8. On how many days in the year were thunderstorms reported? a. 9 b.
16 c. 21 d. 40 9. The strongest gust of wind, as reported in maximum 3-sec wind, was mph. This
occurred in the month of a. 58 August b. 64 August c. 71 July d. 87 July 10. The total
precipitation for the year (water equivalent: total) was in. a. 10.02 b. 15.37 c. 22.98 d. 39.21
11. The total number of days with at least a trace of precipitation (equal or greater than 0.01in.)
was a. 4 b. 37 c. 72 d. 109 12. The total number of days in 2020 when an inch or more of snow
fell was a. 2 b. 8 c. 15 d. 21
NORMALS, MEANS, AND EXTREMES
13. According to Figure 2B3, the normal monthly temperatures (normal dry bulb) range from a
low of 25.1F in January to a high of F in July. a. 71.1 b. 73.8 c. 76.2 d. 84.3 14. The highest daily
maximum temperature ever recorded at Grand Island was F in August 1983. a. 99 b. 101 c. 107
d. 110 15. The mean number of days per year with thunderstorms is a. 19.7 b. 32.8 c. 43.3 d. 56.4
16. Over the year the mean wind speed was mph from a direction coded as 17 (tens of degrees
measured clockwise from north), meaning essentially from the south. (Wind from due south
would be coded as 18 .) a. 8.7 b. 11.1 c. 12.9 d. 14.6 17. The normal yearly total precipitation
was in. a. 17.26 b. 21.82 c. 23.42 d. 26.66 18. The total for 2020 was the normal yearly total
precipitation. a. less than b. equal to c. more than
19. Also included as part of the LCD is a description of the location and climate of the area
surrounding the local NWS Forecast Office. According to the Grand Island description in Figure
2B-4, its climate is described as primarily a. maritime b. continental 2020 GRAND ISLAND
NEBRASKA (KGRI) The ctty of Grand Ioland ta located in the shallow The east to vest upalope
vina tlov providea pertode 20-25 nt:es northvest to north of the elty, then by taereased fam
17rigation and so:1 managenent the Yispouri siver vailey in eastem nobraska to the Late opring
and ear1y gumer ia the peak acason tor Roeky Mountatna o: wyontog and Colorado. the e1trate
ta prinari1y continenta1 in.
The weather has been relatively cloudy, warm and dry. We found less debris in the water but saw several large tidal eddies and suspended sediment plumes. Jellyfish continue to go strong this winter. We also observed early algae blooms in Hood Canal and Eld Inlet as well as multiple oil sheens in Seattle waterways. Listen to our marine flight technician discuss EOPS on the radio.
Presented by The Global Peatlands Assessment: Mapping, Policy, and Action at GLF Peatlands 2024 - The Global Peatlands Assessment: Mapping, Policy, and Action
Satellite passive microwave measurements of the climate crisisChelle Gentemann
Invited presentation at the NASEM Committee on Radio Frequencies 2021 Fall Meeting. An overview of how passive microwave measurements are used to understand climate change.
A recent cold spell hits Puget Sound lowlands, interrupting this year’s warmer air temperatures. The warm ocean coincides with new maximum water temperatures observed throughout Puget Sound in October! Hood Canal’s higher dissolved oxygen and cold water anomalies are disappearing. November brings cold water from Whidbey Basin into Puget Sound with moderate levels of chlorophyll fluorescence. Abundant smacks of jellyfish in finger inlets of South Sound observed from our flight. Red-brown blooms remain strong in smaller bays of South Sound. Visible suspended sediments in the coastal estuaries from rain, wind, and waves. Playing in the water? Visit our BEACH program.
Lower than expected air temperatures and sunshine are now both increasing; rivers are generally running high. Willapa Bay unfolds its beauty from a bird’s-eye view. The spring phytoplankton bloom is picking up in Puget Sound. A large red-orange-brown bloom persists in southern Hood Canal at a scale sufficient for the MODIS satellite to pick up. Jellyfish are still going strong in southern inlets. Ocean climate indices (PDO, NPGO and Upwelling Index) explain much of the variability in Puget Sound temperature, salt and oxygen. Nutrients, however, are steadily increasing while sub-surface algal pigments (chlorophyll a) are declining!
After weeks of clouds and warmer air, blue skies and cold temperatures set in. Strong tidal fronts and sediment-rich brackish plumes leave Whidbey Basin and move into Admiralty Reach. A pod of Orcas follows the edge of the plume heading north! Red-brown blooms continue in Henderson, Eld, and northern Budd Inlets. Long organic debris lines are numerous in northern Budd Inlet, Hood Canal, and in Central Sound north of Edmonds (Triple Junction). Conditions in the water column in Puget Sound continue to normalize after seven months of lower oxygen. Water is very clear for this time of the year, particularly in the north.
Impact of Sea Level Rise from Storm Surge USADag Lohmann
We're quantifying the impact that a 30cm sea level rise has on losses from hurricanes for each individual location in the USA. We're also looking at losses from a hypothetical sea level in the year 1900. Summaries are shown by state and selected maps.
Summary of results: Based on current conditions of exposure (e.g. buildings and other economic assets) we have an annual average loss of about $5 Billion from our simulations. Given the sea level in 1900 that loss would go to $4 Billion. Current projections of sea level rise vary widely, but most have us exceed 30cm between 2040 and 2080. Some go much higher (many meters), while the most optimistic ones are around 30cm at the end of the century. Given the same exposure, same sea defenses, and same hurricanes, losses would go up to an average of $6.9 Billion / year (called the average annual loss or AAL).
The pattern of colder and fresher Puget Sound water persists. Jellyfish aggregations continue to persist in Budd Inlet. Debris lines are numerous and long. There are multiple oil sheens in Seattle waterways. CDOM (colored dissolved organic matter) sensor and en route ferry thermosalinograph provide an important tracer for freshwater entering Puget Sound from Whidbey Basin.
Click on Figure 2B-1 to open it in a new browser tab. This works f.pdfbaraeaaa
Click on Figure 2B-1 to open it in a new browser tab. This works for all figures. 1. Frost occurs
if the temperature falls to 32F or lower, so the date of the last spring frost in 2020 at Grand
Island was near May. a. 1 b. 10 c. 22 d. 28 2. The date of the year's first fall frost was on or
around October. a. 1 b. 13 c. 20 d. 29
Figure 2B-2. Grand Island meteorological data for 2020. 3. had the lowest average temperature
(average dry bulb), which was F. a. December 32.3 b. January ... 27.4 c. February 31.9 4. In ,
Grand Isle saw its highest average temperature at F. a. June ...77.6 b. July ... 77.4 c. August ...
79.9 5. How many days in the year had temperatures of 90F or higher? a. 21 b. 23 c. 37 d. 50 6.
How many days had temperatures of 0F or lower? a. 2 b. 17 c. 24 d. 33
7. In 2020 , Grand Island experienced about times more heating degree days than cooling degree
days. a. 2 b. 4 c. 8 d. 10 8. On how many days in the year were thunderstorms reported? a. 9 b.
16 c. 21 d. 40 9. The strongest gust of wind, as reported in maximum 3-sec wind, was mph. This
occurred in the month of a. 58 August b. 64 August c. 71 July d. 87 July 10. The total
precipitation for the year (water equivalent: total) was in. a. 10.02 b. 15.37 c. 22.98 d. 39.21
11. The total number of days with at least a trace of precipitation (equal or greater than 0.01in.)
was a. 4 b. 37 c. 72 d. 109 12. The total number of days in 2020 when an inch or more of snow
fell was a. 2 b. 8 c. 15 d. 21
NORMALS, MEANS, AND EXTREMES
13. According to Figure 2B3, the normal monthly temperatures (normal dry bulb) range from a
low of 25.1F in January to a high of F in July. a. 71.1 b. 73.8 c. 76.2 d. 84.3 14. The highest daily
maximum temperature ever recorded at Grand Island was F in August 1983. a. 99 b. 101 c. 107
d. 110 15. The mean number of days per year with thunderstorms is a. 19.7 b. 32.8 c. 43.3 d. 56.4
16. Over the year the mean wind speed was mph from a direction coded as 17 (tens of degrees
measured clockwise from north), meaning essentially from the south. (Wind from due south
would be coded as 18 .) a. 8.7 b. 11.1 c. 12.9 d. 14.6 17. The normal yearly total precipitation
was in. a. 17.26 b. 21.82 c. 23.42 d. 26.66 18. The total for 2020 was the normal yearly total
precipitation. a. less than b. equal to c. more than
19. Also included as part of the LCD is a description of the location and climate of the area
surrounding the local NWS Forecast Office. According to the Grand Island description in Figure
2B-4, its climate is described as primarily a. maritime b. continental 2020 GRAND ISLAND
NEBRASKA (KGRI) The ctty of Grand Ioland ta located in the shallow The east to vest upalope
vina tlov providea pertode 20-25 nt:es northvest to north of the elty, then by taereased fam
17rigation and so:1 managenent the Yispouri siver vailey in eastem nobraska to the Late opring
and ear1y gumer ia the peak acason tor Roeky Mountatna o: wyontog and Colorado. the e1trate
ta prinari1y continenta1 in.
The weather has been relatively cloudy, warm and dry. We found less debris in the water but saw several large tidal eddies and suspended sediment plumes. Jellyfish continue to go strong this winter. We also observed early algae blooms in Hood Canal and Eld Inlet as well as multiple oil sheens in Seattle waterways. Listen to our marine flight technician discuss EOPS on the radio.
Presented by The Global Peatlands Assessment: Mapping, Policy, and Action at GLF Peatlands 2024 - The Global Peatlands Assessment: Mapping, Policy, and Action
Artificial Reefs by Kuddle Life Foundation - May 2024punit537210
Situated in Pondicherry, India, Kuddle Life Foundation is a charitable, non-profit and non-governmental organization (NGO) dedicated to improving the living standards of coastal communities and simultaneously placing a strong emphasis on the protection of marine ecosystems.
One of the key areas we work in is Artificial Reefs. This presentation captures our journey so far and our learnings. We hope you get as excited about marine conservation and artificial reefs as we are.
Please visit our website: https://kuddlelife.org
Our Instagram channel:
@kuddlelifefoundation
Our Linkedin Page:
https://www.linkedin.com/company/kuddlelifefoundation/
and write to us if you have any questions:
info@kuddlelife.org
Climate Change All over the World .pptxsairaanwer024
Climate change refers to significant and lasting changes in the average weather patterns over periods ranging from decades to millions of years. It encompasses both global warming driven by human emissions of greenhouse gases and the resulting large-scale shifts in weather patterns. While climate change is a natural phenomenon, human activities, particularly since the Industrial Revolution, have accelerated its pace and intensity
UNDERSTANDING WHAT GREEN WASHING IS!.pdfJulietMogola
Many companies today use green washing to lure the public into thinking they are conserving the environment but in real sense they are doing more harm. There have been such several cases from very big companies here in Kenya and also globally. This ranges from various sectors from manufacturing and goes to consumer products. Educating people on greenwashing will enable people to make better choices based on their analysis and not on what they see on marketing sites.
"Understanding the Carbon Cycle: Processes, Human Impacts, and Strategies for...MMariSelvam4
The carbon cycle is a critical component of Earth's environmental system, governing the movement and transformation of carbon through various reservoirs, including the atmosphere, oceans, soil, and living organisms. This complex cycle involves several key processes such as photosynthesis, respiration, decomposition, and carbon sequestration, each contributing to the regulation of carbon levels on the planet.
Human activities, particularly fossil fuel combustion and deforestation, have significantly altered the natural carbon cycle, leading to increased atmospheric carbon dioxide concentrations and driving climate change. Understanding the intricacies of the carbon cycle is essential for assessing the impacts of these changes and developing effective mitigation strategies.
By studying the carbon cycle, scientists can identify carbon sources and sinks, measure carbon fluxes, and predict future trends. This knowledge is crucial for crafting policies aimed at reducing carbon emissions, enhancing carbon storage, and promoting sustainable practices. The carbon cycle's interplay with climate systems, ecosystems, and human activities underscores its importance in maintaining a stable and healthy planet.
In-depth exploration of the carbon cycle reveals the delicate balance required to sustain life and the urgent need to address anthropogenic influences. Through research, education, and policy, we can work towards restoring equilibrium in the carbon cycle and ensuring a sustainable future for generations to come.
Altered Terrain: Colonial Encroachment and Environmental Changes in Cachar, A...PriyankaKilaniya
The beginning of colonial policy in the area was signaled by the British annexation of the Cachar district in southern Assam in 1832. The region became an alluring investment opportunity for Europeans after British rule over Cachar, especially after the accidental discovery of wild tea in 1855. Within this historical context, this study explores three major stages that characterize the evolution of nature. First, it examines the distribution and growth of tea plantations, examining their size and rate of expansion. The second aspect of the study examines the consequences of land concessions, which led to the initial loss of native forests. Finally, the study investigates the increased strain on forests caused by migrant workers' demands. It also highlights the crucial role that the Forest Department plays in protecting these natural habitats from the invasion of tea planters. This study aims to analyze the intricate relationship between colonialism and the altered landscape of Cachar, Assam, by means of a thorough investigation, shedding light on the environmental, economic, and societal aspects of this historical transformation.
Top 8 Strategies for Effective Sustainable Waste Management.pdfJhon Wick
Discover top strategies for effective sustainable waste management, including product removal and product destruction. Learn how to reduce, reuse, recycle, compost, implement waste segregation, and explore innovative technologies for a greener future.
Characterization and the Kinetics of drying at the drying oven and with micro...Open Access Research Paper
The objective of this work is to contribute to valorization de Nephelium lappaceum by the characterization of kinetics of drying of seeds of Nephelium lappaceum. The seeds were dehydrated until a constant mass respectively in a drying oven and a microwawe oven. The temperatures and the powers of drying are respectively: 50, 60 and 70°C and 140, 280 and 420 W. The results show that the curves of drying of seeds of Nephelium lappaceum do not present a phase of constant kinetics. The coefficients of diffusion vary between 2.09.10-8 to 2.98. 10-8m-2/s in the interval of 50°C at 70°C and between 4.83×10-07 at 9.04×10-07 m-8/s for the powers going of 140 W with 420 W the relation between Arrhenius and a value of energy of activation of 16.49 kJ. mol-1 expressed the effect of the temperature on effective diffusivity.
Characterization and the Kinetics of drying at the drying oven and with micro...
FFDI approximation for Sorrento Victoria Australia on Black Saturday
1. APPENDIX XXXX
Black Saturday 7 Feb 2009:
Sorrento Fire Danger Rating and FFDI Evaluation
1. FDR/FFDI Relevance
The CFA advice that “The Fire Danger Rating (FDR) predicts how a fire would behave if one started, including how difficult it would be to put out. The higher the rating, the more dangerous the conditions. The rating is your trigger to act, so to stay safe you need to stay aware of the Fire Danger Rating in your district.”
The FDR bands to set FDR rating of CODE RED, Extreme etc. are equal to the correlation used for the FFDI or “Forest Fire Danger Index”. The Weather Bureau advices the predicted temperature, humidity, wind speed and drought factor when are then used to calculate the FFDI/FDR and are then published to the community.
The CSIRO have studied the statistical relationship between FFDI and house loss in Australia between 1957 and 2009. (Meteorological conditions and wildfire related house loss in Australia between 1957 and 2009 Blanchi et al International Journal of Wildland Fire 2010, 19,914-926).
Key conclusions were that:-
A. Majority of house losses occurred when FFDI>100,
B. Virtually all of the house loss has occurred above the 99.5th percentile level in the distribution of daily FFDI,
C. Little house loss has occurred on days where the FFDI did not exceed 50 suggesting that historical building practices may be maintained in regions where this level is not likely to be exceeded.
Further a statistical review by Leonard (as per below excerpt from “Australia’s revised arrangements for bushfire advice and alerts, AMEC) showed the following house and life loss when correlated with FFDI which clearly shows the elevated risk of house loss and loss of life at higher FFDI’s.
The fire danger rating (FDR) system used by CFA as a state wide warning system directly correlates to FFDI.
2. 2. Sorrento Black Saturday FFDI
The table below shows the number of hours on 7 Feb 2009 for each Fire Danger Rating.
Black Saturday Fire Danger Rating Frequency
Hourly Number of Occurrences
Rye
Sorrento (estimate)
Rhyll (Phillip Island)
Cerberus
Aireys Inlet
Melb Airport
Wallan Catastrophic >100
0
0
0
0 3 5 4 Severe/Extreme 50-100 0 0 1 5 1 4 4 Very High 24-50 1 4 3 0 1 4 2 High 12-24 3 2 2 3 3 4 11 Low & Moderate 0-12 20 18 18 16 16 7 3
> Moderate 4 6 6 8 8 17 21
Rye, Sorrento and Rhyll did not reach Severe/Extreme or Catastrophic and spent a small number of hours at Very High and the rest of the day at High or Moderate. Interestingly the maximum FFDI measured at Rye by Mornington Peninsula Shire Council staff was 25 which lasted for one hour.
As an example the known bushfire areas of (say) Airey’s Inlet and Wallan had FFDI’s in the 150-160 range for extended periods. Also it is interesting to note that Cerberus had high FFDI’s ranging 78-97 which shows that the Fire Risk varies significantly within the same region.
The reason the area between Rye and Sorrento and Phillip Island had low FFDI’s on Victoria’s worst ever extreme fire weather day significant “water fetch” to the north & south which generates much higher humidity and more temperate conditions relative to Victoria inland areas and also coastal areas like Aries Inlet and Cerberus which only have significant land mass to the north. The Google map below illustrates the “water fetch”.
3. 3. Conclusion
FFDI/FDR is used by the CFA as one indicator of fire risk.
On Black Saturday Sorrento, Rhyll and Rye recorded FDR’s significantly lower than known fire areas of Victoria and hence provide a much lower risk of property and loss of life
4. FFDI Black Saturday: Supporting Information
A. Data Assumptions
Note 1
All data is from Bureau of Meteorology except Rye is from Mornington Peninsula Shire Council
Note 2
Humidity, Temperature ex Rhyll as Sorrento and Rhyll are surrounded by water. Because Sorrento has more water to the north it would be expected that humidity would be higher and temperature lower than Rhyll. Cerberus only has land to the North so not appropriate.
Note 3
Windspeed is taken at 25 William Buckley Way with the relationship between South Channel and William Buckley way has been measured using a Davis Weather Station installed at 10m height above the ground over 35 days and 1680 data points. William Buckley Way is 66% on average of South Channel Windspeed across all wind directions.
Note 4
Drought Factor = 10 = worst case, which is probably high for Sorrento given its proximity to the sea and the prevalence of coastal showers
5. B. FFDI for Black Saturday
Table below indicates the extreme conditions inland and also at coastal areas where there is no water mass to the north., eg. Airey’s Inlet and Cerberus. Hence, significantly lower risk at locations like Sorrento, Rye and Rhyll.
Time of Day AESDT, Black Saturday, 7 Feb 2009
Aireys Inlet
Cerberus
Melb Airport
Rhyll
Sorrento Notes 2,3,4
Wallan
Rye Note 3
0 10 4 7 4 2 14 NA
1 6 3 9 3 2 14 NA
2 3 3 23 3 3 15 NA
3 2 2 26 2 2 17 NA
4 2 2 14 4 3 16 NA
5 2 1 5 3 3 15 NA
6 2 2 4 2 3 15 NA
7 2 3 37 4 3 22 NA
8 2 6 64 3 3 30 NA
9 3 10 78 4 4 39 NA
10 11 16 91 8 10 71 4
11 88 78 133 12 17 92 4
12 117 85 133 63 29 159 6
13 145 97 114 47 27 106 9
14 150 85 104 46 40 155 12
15 45 97 83 38 39 131 14
16 15 21 115 21 19 97 16
17 10 9 43 7 7 81 25
18 17 22 39 7 8 16 19
19 18 6 17 4 3 19 10
20 2 5 13 3 2 11 6
21 1 3 10 3 2 8 NA
22 2 2 3 1 1 9 NA
23 7 5 7 5 3 14 NA
6. The table below shows that Sorrento and Rye did not reach catastrophic levels and the hours in excess of Moderate Fire danger are significantly lower than Melbourne and Wallan.
Fire Danger Rating Frequency
Hourly Number of Occurrences
Aireys Inlet
Cerberus
Melb Airport
Rhyll
Sorrento Notes 2,3,4
Wallan
Rye Note 3 Low 0-5 11 11 3 15 15 0 15 Moderate 5-12 5 5 4 3 3 3 5 High 12-24 3 3 4 2 2 11 3 Very High 24-50 1 0 4 3 4 2 1 Extreme 50-100 1 5 4 1 0 4 0 Catastrophic >100 3
0 5
0
0 4 0
> Moderate
8
8
17
6
6
21
4