Showing posts with label Hormozgan Province. Show all posts
Showing posts with label Hormozgan Province. Show all posts

Wednesday, 24 July 2024

Local transmission of Dengue Fever recorded in Iran for the first time.

The transmission of Dengue Fever within Iran has been demonstrated for the first time in June 2024, according to a press release issued by the World Health Organization on 22 July 2024. The Ministry of Health and Medical Education of Iran reported to cases of the disease had been confirmed by Polymerase Chain Reaction testing at the Pasteur Institute in Bandar Abbas, both in patients from the city of Bandar-Lengheh in Hormozgan Province who had never travelled outside of Iran, and who can therefore be confirmed to have acquired the infection within the country. By 17 July 2024 twelve cases had been confirmed in Bandar-Lengheh among people who had no history of travel outside the country.

This development is not entirely unexpected, as the number of imported cases within Iran has remained steady at about 20 per year between 2017 and 2023, and the Aedes aegypti and Aedes albopictus Mosquitoes, which act as vectors for the disease, are both present in Sistan and Balouchistan, Hormozgan, Bushehr, Khuzastan, and Gilan provinces. In 2024 the number of cases in the country has risen sharply, with 137 reported between 15 May and 10 July.

Dengue is a viral infection transmitted to humans through the bite of infected Mosquitoes and is found in tropical and sub-tropical climates worldwide, mostly in urban and semi-urban areas. The primary vectors that transmit the disease are Aedes aegypti Mosquitoes and, to a lesser extent, Aedes albopictus.  These mosquitoes are also vectors of Chikungunya, Yellow Fever and Zika viruses. Dengue is widespread throughout the tropics, with local variations in risk influenced by climate parameters as well as social and environmental factors.

Colour print of the Dengue Mosquito Aedes aegypti (then called Stegomyia fasciata, today also Stegomyia aegypti). To the left, the male, in the middle and on the right, the female. Above left, a flying pair in copula. Emil August Goeldi (1905)/Wikimedia Commons.

Infection with the Dengue Virus can cause a wide spectrum of disease. Ranging from subclinical disease (people may not know they are even infected) to severe flu-like symptoms in those infected. Although less common, some people develop Severe Dengue, which can be any number of complications associated with severe bleeding, organ impairment and/or plasma leakage. Severe Dengue has a higher risk of death when not managed appropriately. Severe Dengue was first recognised in the 1950s during Dengue epidemics in the Philippines and Thailand. Today, Severe Dengue affects most Asian and Latin American countries and has become a leading cause of hospitalisation and death among children and adults in these regions.

Dengue is caused by a Virus of the Flaviviridae family of positive-strand RNA Viruses and there are four distinct, but closely related, serotypes of the Virus that cause Dengue (Dengue Fever Virus-1, Dengue Fever Virus-2, Dengue Fever Virus-3 and Dengue Fever Virus-4). Recovery from infection is believed to provide lifelong immunity against that serotype. However, cross-immunity to the other serotypes after recovery is only partial, and temporary. Subsequent infections (secondary infection) by other serotypes increase the risk of developing Severe Dengue.

A transmission electron micrograph showing Dengue Virus virions (the cluster of dark dots near the centre). Centers for Disease Control and Prevention/Wikimedia Commons.

Dengue has distinct epidemiological patterns, associated with the four serotypes of the Virus. These can co-circulate within a region, and indeed many countries are hyper-endemic for all four serotypes. Dengue has an alarming impact on both human health and the global and national economies. Dengue Fever Virus is frequently transported from one place to another by infected travellers; when susceptible vectors are present in these new areas, there is the potential for local transmission to be established.

The incidence of Dengue has grown dramatically around the world in recent decades. A vast majority of cases are asymptomatic or mild and self-managed, and hence the actual numbers of dengue cases are under-reported. Many cases are also misdiagnosed as other febrile illnesses.

One modelling estimate indicates 390 million Dengue Virus infections per year, of which 96 million manifest clinically (with any severity of disease). Another study on the prevalence of dengue estimates that 3.9 billion people are at risk of infection with dengue viruses. Despite a risk of infection existing in 129 countries, 70% of the actual burden is in Asia.

The number of dengue cases reported to the World Health Organization increased over 8 fold over the last two decades, from 505 430 cases in 2000, to over 2.4 million in 2010, and 5.2 million in 2019. Reported deaths between the year 2000 and 2015 increased from 960 to 4032, affecting mostly younger age group. The total number of cases seemingly decreased during years 2020 and 2021, as well as for reported deaths. However, the COVID-19 pandemic might have also hampered case reporting in several countries.

The overall alarming increase in case numbers over the last two decades is partly explained by a change in national practices to record and report Dengue to the Ministries of Health, and to the World Health Organization. But it also represents government recognition of the burden, and therefore the pertinence to report Dengue disease burden.

Before 1970, only 9 countries had experienced Severe Dengue epidemics. The disease is now endemic in more than 100 countries in the World Health Organization regions of Africa, the Americas, the Eastern Mediterranean, South-East Asia and the Western Pacific. The Americas, South-East Asia and Western Pacific regions are the most seriously affected, with Asia representing about 70% of the global burden of disease.

Not only is the number of cases increasing as the disease spreads to new areas including Europe, but explosive outbreaks are occurring. The threat of a possible outbreak of Dengue now exists in Europe; local transmission was reported for the first time in France and Croatia in 2010 and imported cases were detected in 3 other European countries. In 2012, an outbreak of Dengue on the Madeira islands of Portugal resulted in over 2000 cases and imported cases were detected in mainland Portugal and 10 other countries in Europe. Autochthonous cases are now observed on an annual basis in few European countries.

Iran forms part of the World Health Organization's Eastern Mediterranean Region, which is considered to be at high risk to Dengue Fever epidemics, with many countries having fragile healthcare systems due to conflict and political instability, while other countries where healthcare systems are considered to be stronger are sufferering increased rains due to climate change, leading to a proliferation of the Aedes aegypti and Aedes albopictus Mosquitoes which act as vectors for the disease. 

The countries of the World Health Organization's Eastern Mediterranean Region. Özturk et al. (2024).

Iran is particularly threatened by the presence of both types of Mosquito and a climate favourable to the spread of the disease, as well as a large numbers of visitors from countries where the disease is endemic. The discovery that the disease is being transmitted in the country at this time is particularly alarming as it comes shortly before the annual Arba'in Pilgrimage, which this year will take place in August, with potentially millions of Shiite Muslims from around the world visiting the Shrine of Husayn ibn Ali in the city of Karbala in central Iran.

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Friday, 2 December 2022

Magnitude 5.7 Earthquake in Hormozgan Province, Iran.

The United States Geological Survey recorded a Magnitude 5.7 Earthquake at a depth of 4.7 km roughly 49 km to the northeast of the port of Bandar-e Lengeh in Hormozgan Province, Iran, slightly after 6.45 pm local time (slightly after 3.15 pm GMT) on Wednesday 30 November 2022. There are no reports of any damage or casualties associated with this event, but many people in the United Arab Emirates reported feeling it.

The location of the 30 November 2022 Hormozgan Province Earthquake. USGS.

Iran is situated on the southern margin of the Eurasian Plate. Immediately to the south lies the Arabian Plate, which is being pushed northward by the impact of Africa from the south. This has created a zone of faulting and fold mountains along the southwest coast of the country, known as the Zagros Thrust Belt, while to the northeast of this the geology is dominated by three large tectonic blocks, the Central Iran, Lut and Helmand, which move separately in response to pressure from the south, stretching and compressing the rock layers close to the surface and creating frequent Earthquakes, some of which can be very large.

The movement of the Arabian Plate and extent of the Zagros Thrust Belt. Rasoul Sorkhabi/Geo ExPro.

The population of Iran is particularly at risk from Earthquakes as, unlike most other Earthquake-prone nations, very few buildings in the country are quake-resistant. The majority of residential buildings in Iran are made of mud-brick, a building material particularly vulnerable to Earthquakes as the bricks often liquefy, trapping people inside and quickly asphyxiating them with dust. This is particularly dangerous at night when the majority of people are inside sleeping.

Section through the Zagros Fold Belt. Sarkarinejad & Azizi (2007).

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Tuesday, 26 July 2022

Magnitude 5.4 Earthquake in Hormozgan Province, Iran.

The United States Geological Survey recorded a Magnitude 5.4 Earthquake at a depth of 10.0 km roughly 51 km to the northeast of the port of Bandar-e Lengeh in Hormozgan Province, Iran, slightly after 4.05 pm local time (slightly after 8.35 pm GMT) on Saturday 23 July 2022. There are no reports of any damage or casualties associated with this event, but many people in the United Arab Emirates reported feeling it.

The location of the 23 July 2022 Hormozgan Province Earthquake. USGS.

Iran is situated on the southern margin of the Eurasian Plate. Immediately to the south lies the Arabian Plate, which is being pushed northward by the impact of Africa from the south. This has created a zone of faulting and fold mountains along the southwest coast of the country, known as the Zagros Thrust Belt, while to the northeast of this the geology is dominated by three large tectonic blocks, the Central Iran, Lut and Helmand, which move separately in response to pressure from the south, stretching and compressing the rock layers close to the surface and creating frequent Earthquakes, some of which can be very large.

The movement of the Arabian Plate and extent of the Zagros Thrust Belt. Rasoul Sorkhabi/Geo ExPro.

To the northeast of this the geology is dominated by three large tectonic blocks, the Central Iran, Lut and Helmand, which move separately in response to pressure from the south, stretching and compressing the rock layers close to the surface and again creating frequent Earthquakes.

The population of Iran is particularly at risk from Earthquakes as, unlike most other Earthquake-prone nations, very few buildings in the country are quake-resistant. The majority of residential buildings in Iran are made of mud-brick, a building material particularly vulnerable to Earthquakes as the bricks often liquefy, trapping people inside and quickly asphyxiating them with dust. This is particularly dangerous at night when the majority of people are inside sleeping.

Section through the Zagros Fold Belt. Sarkarinejad & Azizi (2007).

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Tuesday, 24 March 2020

Flooding kills at least thirteen people in southern Iran.

At least thirteen people have died in flooding across southern Iran between Friday 20 and Monday 23 March 2020. The worst of the flooding has been reported in Fars and Hormozgan provinces, each of which have suffered at least five casualties, Bushehr where two deaths have been confirmed, and Qom, which has also recorded a single death, but floods have also occurred in Kerman, Sistan,  Baluchestan, Gilan, Kohgiluyeh & Boyer-Ahmad, and Golestan provinces. Flooding has also been recorded in neighbouring areas of Iraq and Saudi Arabia.

Flooding in southern Iran in March 2020. Jonoub Fouri/Twitter.

The Middle East, while generally arid, is prone to occasional severe flooding. This stems from two causes; firstly the arid climate prevents the development of a thick soil layer which would be expected in less dry areas, so that in much of the area (non-porous) bedrock is either exposed or close to the surface, and secondly the hot climate leads to heavy evaporation from nearby seas and oceans, so that if the wind changes direction and brings water-laden air to the area, it brings a lot of precipitation with it. This combination of heavy rainfall and low ground absorbency leads to large amounts of water at the surface, typically moving downhill at some speed. Wadis, dry channels or ravines through which these sudden floods are channelled, can be particularly dangerous at these times, particularly as they often appear to resemble natural pathways or even camp sites to people unfamiliar with the climate.

Flooding in southern Iran in March 2020. Tasnim News Agency.

The storms have been caused by a low pressure system over the eastern Mediterranean, caused by hot weather in the region, a common problem during spring in the region. As the air is heated the the air pressure drops and the air rises, causing new air to rush in from outside the forming storm zone. If this zone is sufficiently large, then it will be influenced by the Coriolis Effect, which loosely speaking means the winds closer to the equator will be faster than those further away, causing the storm to rotate, clockwise in the northern hemisphere and anticlockwise in the southern hemisphere.

 Debris left by flooding in southern Iran in March 2020. Dobrinich Channel/YouTube.

Whilst the high winds associated these storms is extremely dangerous, the real danger from such storms is often the flooding. Each millibar drop in air pressure can lead to a 1 cm rise in sea level, and large storms can be accompanied by storm surges several meters high. This tends to be accompanied by high levels of rainfall, caused by water picked up by the storm while still at sea, which can lead to flooding, swollen rivers and landslides; which occur when waterlogged soils on hill slopes lose their cohesion and slump downwards, over whatever happens to be in their path.

See also...

https://sciencythoughts.blogspot.com/2019/11/magnitude-59-earthquake-in-east.htmlhttps://sciencythoughts.blogspot.com/2019/10/magnitude-54-earthauke-in-hormozgan.html
https://sciencythoughts.blogspot.com/2019/10/mirabad-e-emam-qoli-sassanid-era-fire.htmlhttps://sciencythoughts.blogspot.com/2019/05/magnitude-41-earthquake-in-hormozgan.html
https://sciencythoughts.blogspot.com/2019/05/tamarix-humboldtiana-new-species-of.htmlhttps://sciencythoughts.blogspot.com/2019/03/former-footballer-killed-by-landslide.html
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Tuesday, 22 October 2019

Magnitude 5,4 Earthauke in Hormozgān Province, Iran.

The United States Geological Survey recorded a Magnitude 5.4 Earthquake at a depth of 10.0 km roughly 73 km to the north of the city of Bandar-e Lengeh in Hormozgān Province, Iran, slightly before 2.00 pm local time (slightly before 11.00 am GMT) on Friday 21 October 2019. There are no reports of any damage or casualties associated with this event, but it was felt across much of southern Iran, as well as in Bahrain and the United Arab Emirates.

The location of the 21 October 2019 Hormozgān Province Earthquake. Contour lines show rates of movement during the quake, the red line is a boundary between two tectonic plates, in this case the Arabian and Eurasian plates. USGS.

Iran is situated on the southern margin of the Eurasian Plate. Immediately to the south lies the Arabian Plate, which is being pushed northward by the impact of Africa from the south. This has created a zone of faulting and fold mountains along the southwest coast of the country, known as the Zagros Thrust Belt, while to the northeast of this the geology is dominated by three large tectonic blocks, the Central Iran, Lut and Helmand, which move separately in response to pressure from the south, stretching and compressing the rock layers close to the surface and creating frequent Earthquakes, some of which can be very large.

 The movement of the Arabian Plate and extent of the Zagros Thrust Belt. Rasoul Sorkhabi/Geo ExPro.

To the northeast of this the geology is dominated by three large tectonic blocks, the Central Iran, Lut and Helmand, which move separately in response to pressure from the south, stretching and compressing the rock layers close to the surface and again creating frequent Earthquakes.

The population of Iran is particularly at risk from Earthquakes as, unlike most other Earthquake-prone nations, very few buildings in the country are quake-resistant. The majority of residential buildings in Iran are made of mud-brick, a building material particularly vulnerable to Earthquakes as the bricks often liquefy, trapping people inside and quickly asphyxiating them with dust. This is particularly dangerous at night when the majority of people are inside sleeping.

Section through the Zagros Fold Belt. Sarkarinejad & Azizi (2007).

Witness accounts of Earthquakes can help geologists to understand these events, and the structures that cause them. The international non-profit organisation Earthquake Report is interested in hearing from people who may have felt this event; if you felt this quake then you can report it to Earthquake Report here.
 
See also...
 
https://sciencythoughts.blogspot.com/2019/10/mirabad-e-emam-qoli-sassanid-era-fire.htmlhttps://sciencythoughts.blogspot.com/2019/05/magnitude-41-earthquake-in-hormozgan.html
https://sciencythoughts.blogspot.com/2019/05/tamarix-humboldtiana-new-species-of.htmlhttps://sciencythoughts.blogspot.com/2019/03/former-footballer-killed-by-landslide.html
https://sciencythoughts.blogspot.com/2018/12/zercon-triangularis-new-species-of.htmlhttps://sciencythoughts.blogspot.com/2018/11/heavy-rains-bring-flooding-to-iran-iraq.html
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Sunday, 12 May 2019

Magnitude 4.1 Earthquake in Hormozgān Province, Iran.

The United States Geological Survey recorded a Magnitude 4.1 Earthquake at a depth of 35.0 km roughly 44 km to the northwest of the city of Bandar 'abbas in Hormozgān Province, Iran, slightly after 7.10 am local time (slightly after 2.40 am GMT) on Friday 10 May 2019. There are no reports of any damage or casualties associated with this event, but it may have been felt locally.

The approximate location of the 10 May 2019 Hormozgān Earthquake. USGS.

Iran is situated on the southern margin of the Eurasian Plate. Immediately to the south lies the Arabian Plate, which is being pushed northward by the impact of Africa from the south. This has created a zone of faulting and fold mountains along the southwest coast of the country, known as the Zagros Thrust Belt, while to the northeast of this the geology is dominated by three large tectonic blocks, the Central Iran, Lut and Helmand, which move separately in response to pressure from the south, stretching and compressing the rock layers close to the surface and creating frequent Earthquakes, some of which can be very large.

 The movement of the Arabian Plate and extent of the Zagros Thrust Belt. Rasoul Sorkhabi/Geo ExPro.

To the northeast of this the geology is dominated by three large tectonic blocks, the Central Iran, Lut and Helmand, which move separately in response to pressure from the south, stretching and compressing the rock layers close to the surface and again creating frequent Earthquakes.

The population of Iran is particularly at risk from Earthquakes as, unlike most other Earthquake-prone nations, very few buildings in the country are quake-resistant. The majority of residential buildings in Iran are made of mud-brick, a building material particularly vulnerable to Earthquakes as the bricks often liquefy, trapping people inside and quickly asphyxiating them with dust. This is particularly dangerous at night when the majority of people are inside sleeping.

 Section through the Zagros Fold Belt. Sarkarinejad & Azizi (2007).

Witness accounts of Earthquakes can help geologists to understand these events, and the structures that cause them. The international non-profit organisation Earthquake Report is interested in hearing from people who may have felt this event; if you felt this quake then you can report it to Earthquake Report here.
 
See also...
 
https://sciencythoughts.blogspot.com/2019/03/former-footballer-killed-by-landslide.htmlhttps://sciencythoughts.blogspot.com/2018/11/heavy-rains-bring-flooding-to-iran-iraq.html
https://sciencythoughts.blogspot.com/2018/10/flooding-kills-at-least-eight-in.htmlhttps://sciencythoughts.blogspot.com/2018/04/magnitude-55-earthquake-in-bushehr.html
https://sciencythoughts.blogspot.com/2017/12/millitant-group-claims-to-have-blown-up.htmlhttp://sciencythoughts.blogspot.co.uk/2017/12/magnitude-49-earthquake-in-tehran.html
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