Graphic showing that we've been in an active period
of tropical cyclone activity since 1995, where the average number of named tropical storms has jumped significantly to 15.2 per year.
Unfortunately, despite this clear empirical evidence, the climate change and global warming doomsday alarmists attempt to portray the 2017 season as a sign of CO2 - induced climate catastrophe - and that is not being well accepted by the actual hurricane experts (here, here, here) who have been on the front lines
of tropical cyclone activity and impact research.
In a study published in the journal Climatic Change, scientists Michael Chenoweth and Dmitry Divine analyze the history
of tropical cyclone activity in the Lesser Antilles from 1638 to 2009.
Now a team from Australia and the Netherlands has analysed stalagmites to create an index
of tropical cyclone activity that stretches back 1500 years.
«Accurate seasonal and decadal predictions
of tropical cyclone activity are essential for the development of mitigation strategies for the 2.7 billion residents living within cyclone prone regions.
Those conditions just tend to be more favorable during the officially recognized six - month season, which encompasses about 97 percent
of tropical cyclone activity in the Atlantic.
The environmental and societal toll makes it important to understand the future
of tropical cyclone activity in this region.
The Accumulated Cyclone Energy (ACE) index
of tropical cyclone activity also indicated a below - average season in the North Atlantic.
Not exact matches
In the Department
of Meteorology at Stockholm University (MISU), researchers have done a series
of model simulations investigating
tropical cyclone activity during an earlier warm climate, the mid-Holocene, 6,000 years ago.
The greening
of Sahara strengthens the West African Monsoon, which triggers a change in the atmospheric circulation over the entire tropics, affecting
tropical cyclone activity.
In a recent study, researchers at the Department
of Meteorology at Stockholm University have found that
tropical cyclone activity may have increased during past warm climates in connection with a greening
of the Sahara.
That signal is translating into all sorts
of events — droughts, intense rainfall, more intense
tropical cyclone activity, crop stress, heat waves, and so on.
The article, «Extreme rainfall
activity in the Australian tropics reflects changes in the El Niño / Southern Oscillation over the last two millennia,» presents a precisely dated stalagmite record
of cave flooding events that are tied to
tropical cyclones, which include storms such as hurricanes and typhoons.
The next meeting will be at the end
of this year and a statement
of the potential changes in
tropical cyclone activity, together with the degree
of uncertainty, will be issued following that meeting.
While the new formula, which accounts for both temperature and salinity, can be used to forecast
tropical cyclone intensity in real time, it can also be applied to the results
of climate modeling to provide scientists with a framework to evaluate changes in future
tropical cyclone activity.
Methods: While a few studies in the past investigated the influence
of climate phenomena such as the El Niño Southern Oscillation and the Madden - Julian Oscillation on the inter-annual variability
of tropical cyclones in the post-monsoon Bay
of Bengal, changes in long - term
cyclone activity are less well understood.
NOAA has issued its annual forecast for the hurricane season, along with its now - standard explanation that there is a natural cycle
of multidecadal (40 - 60 year) length in the North Atlantic circulation (often referred to as the «Atlantic Multidecadal Oscillation» — see Figure), that is varying the frequency
of Atlantic
tropical cyclones, and that the present high level
of activity is due to a concurrent positive peak in this oscillation.
The lesson has a range
of learning
activities suitable to different types
of learners; there are video clips to make real the effects
of tropical cyclones, a picture study task, an interactive task to allow students to move around the room and share their learning and there is a numeracy task for those logical mathematical earners.
Also available in our Natural Disaster
Activity Pack This activity pack contains 14 activities to explore the topic of Tropical Cyclones (which are also called cyclones, hurricanes and typhoons depending upon where you live in the
Activity Pack This
activity pack contains 14 activities to explore the topic of Tropical Cyclones (which are also called cyclones, hurricanes and typhoons depending upon where you live in the
activity pack contains 14
activities to explore the topic
of Tropical Cyclones (which are also called cyclones, hurricanes and typhoons depending upon where you live in the
Cyclones (which are also called
cyclones, hurricanes and typhoons depending upon where you live in the
cyclones, hurricanes and typhoons depending upon where you live in the world).
«Multidecadal variability
of Atlantic
tropical cyclone activity is observed to relate to the Atlantic Multidecadal Oscillation (AMO)-- a mode manifesting primarily in sea surface temperature (SST) in the high latitudes
of the North Atlantic.
Since the climate response to the North Atlantic SST anomalies is primarily forced at the low latitudes and the AWP is in the path
of or a birthplace for Atlantic
tropical cyclones, the influence
of the AMO on Atlantic
tropical cyclone activity may operate through the mechanism
of the AWP - induced atmospheric changes.
By Rasmus Benestad & Michael Mann Just as Typhoon Nargis has reminded us
of the destructive power
of tropical cyclones (with its horrible death toll in Burma — around 100,000 according to the UN), a new paper by Knutson et al in the latest issue
of the journal Nature Geosciences purports to project a reduction in Atlantic hurricane
activity (principally the «frequency» but also integrated measures
of powerfulness).
More specifically, an anomalously large (small) AWP reduces (enhances) the vertical wind shear in the hurricane main development region and increases (decreases) the moist static instability
of the troposphere, both
of which favor (disfavor) Atlantic
tropical cyclone activity.
He cites observations made in Dr. Bill Gray's SUMMARY
OF 2005 ATLANTIC
TROPICAL CYCLONE ACTIVITY for this connection.
While this study is undoubtedly an important contribution to the literature, introducing a potentially useful methodology for refining estimates
of past
tropical cyclone activity in all the major basins, it is hardly the last word (see e.g. the discussion thread in our previous article on the paper).
The clear seasonality in TCs («hurricane season») with highest
activities during the summer is one
of the strongest pieces
of empirical evidence that higher temperatures give more favourable conditions for
tropical cyclones (After all, TCs only form in the warm tropics...).
NOAA also forecasts a high hurricane
activity for the remainder
of the season, and time will show if this season will match the 2004 in terms
of number
of tropical cyclones.
Part
of the difficulty in identifying the human component, if any is, as the IPCC Summary itself notes, that
tropical cyclone activity varies naturally over the decades.
The uncertainties in the historical
tropical cyclone records, the incomplete understanding
of the physical mechanisms linking
tropical cyclone metrics to climate change, and the degree
of tropical cyclone variability provide only low confidence for the attribution
of any detectable changes in
tropical cyclone activity to anthropogenic influences.
Adam G: You can not conclude that just from looking at a basin which has less than 15 %
of the total global
tropical cyclone activity, and also selecting groups
of years that coincide exactly with the positive and negative Atlantic Multi-decadal Oscillation phases, which would dominate over any AGW trend in this basin if it exists.
It adds this substantial cautionary note, however: that «multi-decadal variability and the quality
of the
tropical cyclone records prior to routine satellite observations in about 1970 complicate the detection
of long - term trends in
tropical cyclone activity.»
Accumulated
cyclone energy (ACE) is a measure used by the National Oceanic and Atmospheric Administration (NOAA) to express the
activity of individual
tropical cyclones and entire
tropical cyclone seasons, * particularly the North Atlantic hurricane season.
On the other hand, I don't know if there are correlation studies
of the
cyclone activity with the surface insolation trends in past decades and for each
tropical bassin.
Multi-decadal variability and the quality
of the
tropical cyclone records prior to routine satellite observations in about 1970 complicate the detection
of long - term trends in
tropical cyclone activity.
There is observational evidence for an increase
of intense
tropical cyclone activity in the North Atlantic since about 1970, correlated with increases in
tropical SSTs.
• What are some other impacts
of climatic variability during the MCA / MWP regarding such topics as changes in ocean basin
tropical cyclone activity?
Influence
of Pacific Decadal Oscillation on the relationship between ENSO and
tropical cyclone activity in the Bay
of Bengal during October — December The relationship between ENSO and
tropical cyclones (TCs)
activity in the Bay
of Bengal (BoB) during October — December under cold (1950 — 1974) and warm (1975 — 2006) phase
of Pacific Decadal Oscillation (PDO) is investigated.
The US CLIVAR Hurricane Working Group was formed to improve understanding
of interannual variability and trends in the
tropical cyclone activity from the beginning
of the 20th century to the present and quantify changes in the characteristics
of tropical cyclones under a warming climate.
The development
of a new
tropical cyclone activity index spanning the last 1500 years has enabled the examination
of tropical cyclone climatology at higher temporal resolution than was previously possible.
«The IPCC hierarchy had its mind made up years ago to make every attempt possible to link rising levels
of CO2 with increases in global hurricane intensity and frequency... Input from skeptics or any hypothesis or data that did not link rises in CO2 to increases in
tropical cyclone activity was to be avoided, suppressed, or rejected.»
an improved understanding
of interannual variability and trends in the
tropical cyclone activity from the beginning
of the 20th century to the present
His research
activities revolve around
tropical cyclone simulations and prediction models, 3D and 4D variational analysis schemes, ensemble forecasting techniques and coupling
of mesoscale Numerical Weather Prediction (NWP) models to Atmospheric Transport and Dispersion (ADT) models.
I note that the recent paper shows a dramatic uptick in storm
activity that has been convincingly refuted by «strong evidence that there has been no systematic change in the number
of north Atlantic
tropical cyclones during the 20th century.»
Global
tropical cyclone activity is near historic lows, the frequency
of major U.S. hurricanes has declined, and big tornados have dramatically declined since the 1970s.
Tropical cyclone activity and intensity increasing Record droughts, floods, heat waves, cold spells, high tides occurring Unequivocal warming
of the climate system observed with very high confidence that human
activities are to blame Temperature rising even more dramatically in Arctic, threatening ice loss and extinction
of species Halving human CO2 emissions immediately might save the planet from catastrophe.
WWLLN - TC users can access four categories
of images to follow the lightning
activity and satellite observations
of tropical cyclones:
This means that the potential devastation and destruction that could be caused by
tropical cyclones will get worse and worse in the future, regardless
of any change in
cyclone activity.
[8] In the north Atlantic and the northeastern Pacific oceans,
tropical waves move along the axis
of the ITCZ causing an increase in thunderstorm
activity, and under weak vertical wind shear, these clusters
of thunderstorms can become
tropical cyclones.
The effects
of tropical cyclones early in the year were followed by regular northwest cloud - band
activity between May and mid-July, when waters northwest
of the continent were unusually warm as part
of a negative phase
of the Indian Ocean Dipole.
The Australian monsoon exhibits large interannual and intra-seasonal variability, largely associated with the effects
of ENSO, the Madden - Julian Oscillation (MJO) and
tropical cyclone activity (McBride, 1998; Webster et al., 1998; Wheeler and McBride, 2005).