1961 Atlantic hurricane season

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from:17/07/1961 till:24/07/1961 color:C2 text:Anna (C2)

from:02/09/1961 till:10/09/1961 color:C4 text:Betsy (C4)

from:03/09/1961 till:13/09/1961 color:C4 text:Carla (C4)

from:05/09/1961 till:14/09/1961 color:C1 text:Debbie (C1)

from:10/09/1961 till:26/09/1961 color:C5 text:Esther (C5)

from:12/09/1961 till:15/09/1961 color:TS text:Six (TS)

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from:30/09/1961 till:08/10/1961 color:C4 text:Frances (C4)

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from:17/10/1961 till:20/10/1961 color:TS text:Gerda (TS)

from:26/10/1961 till:01/11/1961 color:C5 text:Hattie (C5)

from:02/11/1961 till:10/11/1961 color:C1 text:Jenny (C1)

from:04/11/1961 till:08/11/1961 color:TS text:Inga (TS)

from:17/11/1961 till:20/11/1961 color:TS text:Twelve (TS)

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from:01/08/1961 till:01/09/1961 text:August

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File:Hurricane_carla_radar.jpg radar image of Hurricane Carla out of Galveston, Texas on September 10]]

The Atlantic hurricane season officially began on June 15.{{cite news|url=https://www.newspapers.com/clip/71391342/the-miami-herald/|title=Scientists Preparing To Break 'Cane's Back|author=E. V. W. Jones|date=June 11, 1961|page=20-A|newspaper=Miami Herald|access-date=February 18, 2021|via=Newspapers.com}} {{free access}} It was an above average season in which twelve tropical storms formed; this was above the 1950–2000 average of 9.6 named storms.{{cite report|author=Philip J. Klotzbach |author2=William M. Gray |date=December 8, 2006 |title=Extended Range Forecast of Atlantic Seasonal Hurricane Activity and U.S. Landfall Strike Probability for 2007 |publisher=Colorado State University |access-date=March 28, 2014 |url=http://hurricane.atmos.colostate.edu/forecasts/2006/dec2006/ |archive-url=https://web.archive.org/web/20061218105454/http://hurricane.atmos.colostate.edu/forecasts/2006/dec2006/ |archive-date=December 18, 2006 |url-status=dead |location=Boulder, Colorado }} Eight of these reached hurricane status, also above of the 1950–2000 average of 5.9.{{Atlantic hurricane best track}} Furthermore, five storms reached major hurricane status. It was originally believed that the season had seven major hurricanes, though later analysis resulted in a downgrade of two storms. Of the five major hurricanes, two became Category 5 hurricanes. Four hurricanes and two tropical storms made landfall during the season,{{Atlantic hurricane best track}} causing 348 deaths and $391.6 million in damage.{{cite report

|url = http://www.aoml.noaa.gov/general/lib/lib1/nhclib/mwreviews/1961.pdf

|title = The Hurricane Season of 1961

|author = Gordon E. Dunn

|date = March 1962

|work = United States Weather Bureau

|publisher = National Oceanic and Atmospheric Administration; Atlantic Oceanographic and Meteorological Laboratory

|access-date = January 31, 2014

|location = Miami, Florida

}}

• {{cite report

|url = http://www1.ncdc.noaa.gov/pub/orders/IPS-9FF6F836-52BD-4912-9F1F-2C5B28F9E210.pd

|title = Storm Data And Unusual Weather Phenomena: September 1961

|author = Luther Hodges

|date = 1961

|work = United States Department of Commerce

|pages = 99–101, 103

|publisher = National Climatic Data Center; National Oceanic and Atmospheric Administration

|access-date = February 1, 2014

|format = PDF

|location = Asheville, North Carolina

|archive-url = https://web.archive.org/web/20140201051314/http://www1.ncdc.noaa.gov/pub/orders/IPS-9FF6F836-52BD-4912-9F1F-2C5B28F9E210.pdf

|archive-date = February 1, 2014

}}

• {{cite report

|url = http://www1.ncdc.noaa.gov/pub/orders/IPS-52F4B7BD-1C8E-49D5-8E58-2306A1702BBA.pdf

|title = Storm Data and Unusual Weather Phenomena: December 1961

|author = Luther Hodges

|work = United States Department of Commerce

|page = 120

|publisher = National Climatic Data Center; National Oceanic and Atmospheric Administration

|location = Asheville, North Carolina

|access-date = February 1, 2014

|archive-url = https://web.archive.org/web/20140201052024/http://www1.ncdc.noaa.gov/pub/orders/IPS-52F4B7BD-1C8E-49D5-8E58-2306A1702BBA.pdf

|archive-date = February 1, 2014

}}

• {{cite news|newspaper=Irish Independent|date=September 18, 1961|title=Gale Killed Fifteen|page=3}} {{subscription required|via=Irish Newspaper Archives}}
• {{cite report

|publisher = Met Éireann

|year = 2012

|access-date = March 28, 2014

|title = Exceptional Weather Events - "Hurricane Debbie"

|url = http://www.met.ie/climate-ireland/weather-events/Sep1961_hurricane-Debbie.pdf

|archive-url = https://web.archive.org/web/20131112040048/http://www.met.ie/climate-ireland/weather-events/Sep1961_hurricane-Debbie.pdf

|archive-date = November 12, 2013

|url-status = dead

|df = mdy-all

}}

• {{cite report

|url = http://www.ss346.com/PDFs/ImhofRescue1961.pdf

|title = Rescue at Sea

|access-date = March 28, 2014

|author = Patrick J. Imhof

|pages = 4–6

|date = September 13, 2005

|location = Pensacola, Florida

|url-status = dead

|archive-url = https://web.archive.org/web/20120204203444/http://www.ss346.com/PDFs/ImhofRescue1961.pdf

|archive-date = February 4, 2012

|df = mdy

}}

• {{cite news

|url = http://www.nhc.noaa.gov/archive/storm_wallets/atlantic/atl1961/gerda/news/savannah.gif

|title = Floods Fatal To 5 Jamaicans

|date = October 20, 1961

|agency = Associated Press

|newspaper = Savannah Morning News

|page = 5

|access-date = August 18, 2013

|location = Kingston, Jamaica

}}

• {{cite press release

|title = Belize Marked 45th Anniversary of Deadly Hurricane Hattie

|url = http://www.nemo.org.bz/cgi-bin/nemonews/exec/view.cgi?archive=1&num=285

|work = Belize National Emergency Management Organization (NEMO)

|access-date = December 3, 2012

|publisher = NEMO Press Officer

|archive-url = https://www.webcitation.org/6Ce1gvhur?url=http://www.nemo.org.bz/cgi-bin/nemonews/exec/view.cgi?archive=1&num=285

|archive-date = December 3, 2012

|date = November 2, 2006

|url-status = dead

}} Hurricane Debbie also caused damage and deaths, despite remaining offshore and then after becoming extratropical.

Tropical cyclogenesis began with an initially unclassified tropical depression, which developed on June 10. More than a month later, Hurricane Anna formed on July 17 and dissipated on July 24. Thereafter, no other systems developed in July or the month of August.{{Atlantic hurricane best track}} A lack of cyclonic activity in the Atlantic basin in August is rare, with such phenomenon not occurring again until the 1997 and 2022 seasons.{{cite news|url=https://www.washingtonpost.com/climate-environment/2022/08/25/august-may-pass-without-single-named-tropical-storm-atlantic/|title=August may pass without a single named tropical storm in the Atlantic|author=Matthew Cappuci|date=August 25, 2022|newspaper=The Washington Post|accessdate=August 28, 2022}} The Atlantic basin remained dormant until Hurricane Betsy developed on September 2. During the next four days, two other tropical cyclones formed – Carla and Debbie. On September 11, the three storms – Betsy, Carla, and Debbie – existed simultaneously as hurricanes,{{Atlantic hurricane best track}} the most in a single day since 1893 and until 1998.{{cite report|url=http://www.aoml.noaa.gov/hrd/tcfaq/E18.html|title=Subject: E18) What was the largest number of hurricanes in the Atlantic Ocean at the same time?|author=Christopher W. Landsea|work=Hurricane Research Division|publisher=National Oceanic and Atmospheric Administration; Atlantic Oceanographic and Meteorological Laboratory|access-date=August 31, 2021|location=Miami, Florida|archive-url=https://web.archive.org/web/20170701034516/http://www.aoml.noaa.gov/hrd/tcfaq/E18.html|archive-date=July 1, 2017}} Esther, which developed on September 10, did not reach hurricane status until September 12. Later that day, a tropical storm that went unnamed formed over the Bahamas and moved across the East Coast of the United States for its brief duration.{{Atlantic hurricane best track}}

After Debbie became extratropical on September 14, another tropical cyclone developed over two weeks later, Hurricane Frances. Thereafter, tropical cyclogenesis slowed in October, which featured only three systems, a second previously unclassified tropical depression, Gerda, and Hattie. The latter was the strongest tropical cyclone of the season, peaking with maximum sustained winds of {{convert|165|mph|km/h|abbr=on}} and a minimum barometric pressure of {{convert|914|mbar|inHg|abbr=on|lk=on}}. After weakening slightly, Hattie struck Belize on October 31, before dissipating on November 1. Later that day, Hurricane Jenny developed northeast of Antigua. Jenny remained weak for much of its duration and became extratropical on November 8. The final system, Tropical Storm Inga, formed in the Gulf of Mexico on November 4. Four days later, Inga dissipated,{{Atlantic hurricane best track}} one week before the season officially ended.

The season's activity was reflected with an accumulated cyclone energy (ACE) rating of 189, one of the highest values recorded. ACE is, broadly speaking, a measure of the power of the hurricane multiplied by the length of time it existed, so storms that last a long time, as well as particularly strong hurricanes, have high ACEs. It is only calculated for full advisories on tropical systems at or exceeding {{convert|39|mph|km/h|abbr=on}}, which is the threshold for tropical storm strength.{{cite report|work=Hurricane Research Division; Atlantic Oceanographic and Meteorological Laboratory|publisher=National Oceanic and Atmospheric Administration|date=March 2011|title=Atlantic basin Comparison of Original and Revised HURDAT|access-date=March 6, 2012|url=http://www.aoml.noaa.gov/hrd/hurdat/comparison_table.html}}

{{Infobox Hurricane Small

| Basin = Atl

| Image = Hurricane Anna 1961.JPG

| Track = Anna 1961 track.png

| Formed = July 17

| Dissipated = July 24

| 1-min winds = 90

| Pressure = 976

}}

{{Main|Hurricane Anna (1961)}}

A tropical wave that emerged into the Atlantic from the west coast of Africa around mid-July developed about {{convert|575|mi|km|abbr=on|round=5}} northeast of Cayenne, French Guiana, late on July 17.{{cite web|url=https://www.aoml.noaa.gov/hrd/hurdat/metadata-1961-1965.pdf|title=1961 Atlantic Hurricane Database Reanalysis|date=2019|author=Christopher W. Landsea|author2=Sandy Delgado|publisher=Atlantic Oceanographic and Meteorological Laboratory|access-date=May 3, 2021|location=Miami, Florida|format=PDF}}{{rp|2}}{{Atlantic hurricane best track}} The depression moved west-northwestward and by the following day, it intensified into a Tropical Storm Anna. After passing just south of Grenada early on July 20, Anna entered the Caribbean Sea. Favorable environmental conditions allowed Anna to reach hurricane intensity late on July 20. The cyclone continued to slowly intensifying, reaching Category 2 intensity on July 22 and peaking with maximum sustained winds of {{convert|105|mph|km/h|abbr=on}}. However, the storm weakened slightly before making landfall as a Category 1 hurricane in Honduras near Barra Patuca, Gracias a Dios Department, with winds of {{convert|80|mph|km/h|abbr=on}}. After re-emerging into the Caribbean, Anna weakened slightly further, striking Utila around 01:00 UTC on July 24 with winds of {{convert|75|mph|km/h|abbr=on}}. About nine hours later, the hurricane made landfall in Belize near Monkey River Town at the same intensity. Anna rapidly weakened over land and dissipated late on July 24.{{Atlantic hurricane best track}}

As a developing tropical cyclone over the Windward Islands, Anna produced strong winds on Grenada, though damage was limited to some crops, trees, and telephone poles.{{cite news|newspaper=The Daily Gleaner|year=1961|title=Anna Should Miss Jamaica}} Other islands experienced gusty winds, but no damage. Passing just north of Venezuela, the hurricane produced strong winds over the country, peaking as high as {{convert|70|mph|km/h|abbr=on}}.{{cite report|url=http://www.nhc.noaa.gov/archive/storm_wallets/atlantic/atl1961/anna/preloc/pshsju02.gif|title=Report on Hurricane Anna – July 20, 1961|author=Ralph L. Higgs|date=August 4, 1961|work=U.S. Weather Bureau Office San Juan, Puerto Rico|publisher=National Oceanic and Atmospheric Administration; National Hurricane Center|page=2|access-date=December 2, 2013|location=San Juan, Puerto Rico}} Strong winds caused widespread damage in northern Honduras. Throughout the country, at least 36 homes were destroyed and 228 were damaged.{{cite report|url=http://www.nhc.noaa.gov/archive/storm_wallets/atlantic/atl1961/anna/preloc/pshmhtg.gif|title=Report on Hurricane Anna|author1=Etat |author2=Gordon E. Dunn |date=August 4, 1961|work=U.S. Weather Bureau Office Miami, Florida|publisher=National Oceanic and Atmospheric Administration; National Hurricane Center|page=11|access-date=December 3, 2013|location=Miami, Florida}} Severe damage in the Gracias a Dios Department left hundreds of people homeless.{{cite news|publisher=National Oceanic and Atmospheric Administration; National Hurricane Center|year=1961|title=Miami Gets Pelted With Short Storms|access-date=December 3, 2013|url=http://www.nhc.noaa.gov/archive/storm_wallets/atlantic/atl1961/anna/news/miami.gif}} Additionally, high winds toppled approximately 10,000 coconut trees. Overall, Anna caused one fatality and $300,000 in damage, primarily in Central America.{{cite report|url=http://www.aoml.noaa.gov/general/lib/lib1/nhclib/mwreviews/1961.pdf|title=The Hurricane Season of 1961|author=Gordon E. Dunn|date=March 1962|work=United States Weather Bureau|publisher=National Oceanic and Atmospheric Administration; Atlantic Oceanographic and Meteorological Laboratory|access-date=January 31, 2014|location=Miami, Florida}}

{{Clear}}

{{Infobox Hurricane Small

| Basin = Atl

| Image = Hurricane Betsy 1961.JPG

| Track = Betsy 1961 track.png

| Formed = September 2

| Dissipated = September 11

| 1-min winds = 115

| Pressure = 945

}}

In early September, a tropical wave was noted in the Intertropical Convergence Zone (ITCZ).{{cite report|title=Hurricane Betsy, September 2-11, 1961|url=http://docs.lib.noaa.gov/rescue/hurricanes/QC9452B472H81961.pdf|location=Miami, Florida|work=United States Weather Bureau|publisher=National Oceanic and Atmospheric Administration|access-date=February 1, 2014}} On September 2, the disturbance was analyzed to have attained tropical storm strength, after nearby ship reports indicated strong winds associated with anomalously low barometric pressures. Moving steadily northwestward, favorable conditions allowed Betsy to quickly intensify later that day.{{Atlantic hurricane best track}} Shortly after, a trough situated along 50°W steered Betsy to a more northerly course. Another low-pressure area later formed in the trough, perturbing the ridge to the north of Betsy for much of its initial stages, causing the hurricane's central pressure to rise, despite an increase in sustained winds.{{Atlantic hurricane best track}} However, on September 5, a shortwave forced the low northeastward, allowing for Betsy to strengthen further.

Early on September 6, Betsy attained Category 4 hurricane strength, peaking with maximum sustained winds of {{convert|130|mph|km/h|abbr=on}} and a central pressure of {{convert|945|mbar|hPa inHg|abbr=on}},{{Atlantic hurricane best track}} based on reconnaissance flights into the system.{{rp|15–16}} However, as a result of missing the short wave itself, the hurricane later weakened and fell to Category 3 intensity while located about {{convert|440|mi|km}} east-northeast of Bermuda. Betsy weakened further to Category 2 hurricane before becoming nearly stationary beginning on September 6. Moving into higher latitudes, Betsy began to weaken, degenerating back to Category 1 hurricane intensity on late on September 8.{{Atlantic hurricane best track}} A separate, minor trough was later able to move the system northeastwards by the following day. Betsy re-intensified into a Category 2 hurricane early on September 10, but transitioned into extratropical cyclone several hours later. The extratropical remnants continued northeastward and weakened, before executing a large loop over the far north Atlantic. The remnants dissipated well north of the Azores on September 16.{{Atlantic hurricane best track}}

{{clear}}

{{Infobox Hurricane Small

| Basin = Atl

| Image = Hurricane Carla Satellite.JPG

| Track = Carla 1961 track.png

| Formed = September 3

| Dissipated = September 13

| 1-min winds = 125

| Pressure = 927

}}

{{Main|Hurricane Carla}}

{{see also|Hurricane Carla tornado outbreak}}

A tropical depression developed from an area of squally weather embedded within the ITCZ in the southwestern Caribbean Sea on September 3.{{cite report|url=http://www.nhc.noaa.gov/archive/storm_wallets/atlantic/atl1961/carla/preloc/new12.gif|title=Carla Preliminary Report|author=ECH|date=September 21, 1961|work=United States Weather Bureau|publisher=National Hurricane Center; National Oceanic and Atmospheric Administration|page=12|access-date=February 1, 2014|location=New Orleans, Louisiana}} Initially a tropical depression, it strengthened slowly while heading northwestward, and by September 4, the system was upgraded to Tropical Storm Carla.{{Atlantic hurricane best track}} About 24 hours later, Carla was upgraded to a hurricane.{{cite report|url=http://www.nhc.noaa.gov/archive/storm_wallets/atlantic/atl1961/carla/preloc/new14.gif|title=Carla Preliminary Report|author=ECH|date=September 21, 1961|work=United States Weather Bureau|publisher=National Hurricane Center; National Oceanic and Atmospheric Administration|page=14|access-date=February 1, 2014|format=GIF|location=New Orleans, Louisiana}} Shortly thereafter, the storm curved northward while approaching the Yucatán Channel. Late on September 7, Carla entered the Gulf of Mexico while passing just northeast of the Yucatán Peninsula. The cyclone reached major hurricane intensity around 12:00 UTC on the next day. Resuming its northwestward course, Carla continued intensification and on September 11, it peaked as a Category 4 hurricane. Carla made landfall near Port O'Connor, Texas, with winds of {{convert|145|mph|km/h|abbr=on}}. It weakened quickly inland and was reduced to a tropical storm on September 12. Heading generally northward, Carla transitioned into an extratropical cyclone on September 13, while centered over southern Oklahoma. However, the remnants continued generally northeastward and entered Canada on September 14, before dissipating near Cape Chidley early on September 16.{{Atlantic hurricane best track}}

While crossing the Yucatán Channel, the outer bands of Carla brought gusty winds and severe local flooding in western Cuba and the Yucatán Peninsula.{{cite news|url=https://www.newspapers.com/clip/69488105/the-miami-news/|title=Hurricane Whips Cuba; Winds Batter Key West|page=72|date=September 7, 1961|newspaper=The Miami News|access-date=February 7, 2021|via=Newspapers.com}} {{free access}} Although initially considered a significant threat to Florida,{{cite report|url=http://www.nhc.noaa.gov/archive/storm_wallets/atlantic/atl1961/carla/public/tcp0710z.gif|title=Hurricane Advisory Number 15 Carla|author=Conner|date=September 7, 1961|work=Weather Bureau Office New Orleans, Louisiana|publisher=National Hurricane Center; National Oceanic and Atmospheric Administration|access-date=February 1, 2014}} the storm brought only light winds and small amounts of precipitation, reaching no more than {{convert|3.15|in|mm|abbr=on}}. In Texas, wind gusts as high as {{convert|170|mph|km/h|abbr=on}} were observed in Port Lavaca. Additionally, several tornadoes spawned in the state caused notable impacts, with the most destructive tornado striking Galveston, Texas at F4 intensity, resulting in 200 buildings being severely damaged, of which 60-75 were destroyed, eight deaths and 200 injuries.{{cite report|url=http://www.nhc.noaa.gov/archive/storm_wallets/atlantic/atl1961/carla/preloc/pshaus1.gif|title=Hurricane Carla in Texas September 8 to 13th, 1961|author=Robert Orton|date=September 16, 1961|work=Weather Bureau Office Galveston, Texas|publisher=National Hurricane Center; National Oceanic and Atmospheric Administration|page=1|access-date=January 11, 2013}} Throughout the state, Carla destroyed 1,915 homes, 568 farm buildings, and 415 other buildings. Additionally, 50,723 homes, 5,620 farm buildings, and 10,487 other buildings suffered damage. There were 34 fatalities and at least $300 million in losses in Texas alone. Several tornadoes also touched down in Louisiana, causing the destruction of 140 homes and 11 farms and other buildings, and major damage to 231 additional homes and 11 farm and other buildings. Minor to moderate damage was also reported to 748 homes and 75 farm and other buildings.{{cite report|url=http://www.nhc.noaa.gov/archive/storm_wallets/atlantic/atl1961/carla/preloc/pshaus.gif|title=List of known dead in Texas from Hurricane Carla as of September 18th|author=Robert Orton|date=September 18, 1961|work=Weather Bureau Office Galveston, Texas|publisher=National Hurricane Center; National Oceanic and Atmospheric Administration|access-date=February 1, 2014}} Six deaths and $25 million in losses in Louisiana were attributed to Carla.{{cite report|url=http://www.nhc.noaa.gov/archive/storm_wallets/atlantic/atl1961/carla/prenhc/prelim2.gif|title=Hurricane Carla: September 4–14, 1961 (A Preliminary Report)|date=September 18, 1961|work=United States Weather Bureau|publisher=National Hurricane Center; National Oceanic and Atmospheric Administration|page=2|access-date=February 1, 2014|location=Miami, Florida}} Heavy rainfall occurred in several other states, especially in Kansas,{{cite report|url=http://www.wpc.ncep.noaa.gov/tropical/rain/tcmidwest.html|title=Tropical Cyclone Rainfall for the Midwest|date=2013|publisher=Weather Prediction Center; National Oceanic and Atmospheric Administration|access-date=February 1, 2014|location=College Park, Maryland}} where flash flooding severely damaged crops and drowned five people.{{cite report|url=http://www1.ncdc.noaa.gov/pub/orders/IPS-9FF6F836-52BD-4912-9F1F-2C5B28F9E210.pd|title=Storm Data And Unusual Weather Phenomena: September 1961|author=Luther Hodges|date=1961|work=United States Department of Commerce|pages=99–101, 103|publisher=National Climatic Data Center; National Oceanic and Atmospheric Administration|access-date=February 1, 2014|format=PDF|location=Asheville, North Carolina|archive-url=https://web.archive.org/web/20140201051314/http://www1.ncdc.noaa.gov/pub/orders/IPS-9FF6F836-52BD-4912-9F1F-2C5B28F9E210.pdf|archive-date=February 1, 2014}} Overall, Carla resulted in $325.74 million in losses and 46 fatalities.{{cite report|url=http://www1.ncdc.noaa.gov/pub/orders/IPS-52F4B7BD-1C8E-49D5-8E58-2306A1702BBA.pdf|title=Storm Data and Unusual Weather Phenomena: December 1961|author=Luther Hodges|work=United States Department of Commerce|page=120|publisher=National Climatic Data Center; National Oceanic and Atmospheric Administration|location=Asheville, North Carolina|access-date=February 1, 2014|archive-url=https://web.archive.org/web/20140201052024/http://www1.ncdc.noaa.gov/pub/orders/IPS-52F4B7BD-1C8E-49D5-8E58-2306A1702BBA.pdf|archive-date=February 1, 2014}} In Canada, the remnants of Carla brought strong winds to Ontario and New Brunswick, though impact was primarily limited to power outages and falling trees and branches.{{cite report|url=http://www.ec.gc.ca/hurricane/default.asp?lang=En&n=9D9BF402-1|title=1961-Carla|date=November 5, 2009|publisher=Environment Canada|access-date=April 3, 2014|location=Fredericton, New Brunswick|archive-url=https://web.archive.org/web/20130703044445/http://www.ec.gc.ca/hurricane/default.asp?lang=En&n=9D9BF402-1|archive-date=July 3, 2013|url-status=live}}

{{clear}}

{{Infobox Hurricane Small

| Basin = Atl

| Image = Hurricane Debbie on September 7, 1961.png

| Track = Debbie 1961 track.png

| Formed = September 5

| Dissipated = September 16

| 1-min winds = 80

| Pressure = 975

}}

{{Main|Hurricane Debbie (1961)}}

A tropical disturbance was first identified in late August over Central Africa.{{cite report|author=C. O. Erickson|publisher=National Oceanic and Atmospheric Administration|date=February 1963|access-date=August 31, 2021|title=An Incipient Hurricane Near The West African Coast|pages=61–68|url=https://journals.ametsoc.org/view/journals/mwre/91/2/1520-0493_1963_091_0061_aihntw_2_3_co_2.xml?tab_body=pdf|location=Miami, Florida|format=PDF}} The wave developed into a tropical depression just offshore Senegal around 12:00 UTC on September 5. It was estimated to have intensified into Tropical Storm Debbie early the next day. Several hours later, Debbie passed through the southern Cape Verde Islands as a strong tropical storm or minimal hurricane,{{Atlantic hurricane best track}} resulting in a plane crash and the death of 60 people.{{cite report|publisher=Met Éireann|year=2012|access-date=March 28, 2014|title=Exceptional Weather Events - "Hurricane Debbie"|url=http://www.met.ie/climate-ireland/weather-events/Sep1961_hurricane-Debbie.pdf|archive-url=https://web.archive.org/web/20131112040048/http://www.met.ie/climate-ireland/weather-events/Sep1961_hurricane-Debbie.pdf|archive-date=November 12, 2013|url-status=dead|df=mdy-all}} Once clear of the islands, data on the storm became sparse, and the status of Debbie was uncertain over the following several days as it tracked west-northwestward and later northward. It was not until a commercial airliner intercepted the storm on September 10 that its location was certain.{{cite report|url=http://docs.lib.noaa.gov/rescue/hurricanes/Qc9452d393h81961.pdf|title=Hurricane Debbie — September 7–15, 1961 Preliminary Report|year=1961|work=National Weather Bureau|publisher=National Oceanic and Atmospheric Administration|access-date=February 5, 2014|location=Miami, Florida}} The following day, Debbie intensified and reached its peak intensity as a strong Category 1 hurricane with maximum sustained winds of {{convert|90|mph|km/h|abbr=on}}. The hurricane gradually slowed its forward motion and weakened.{{Atlantic hurricane best track}} By September 13, Debbie's motion became influenced by the westerlies, causing the system to accelerate east-northeastward. The storm transitioned into an extratropical cyclone late on September 14 about {{convert|140|mi|km|abbr=on|round=5}} west-southwest of Horta, Azores.{{Atlantic hurricane best track}}

The remnants of Debbie soon passed east-northeastward throughout the Azores and then curved northeastward. The system deepened slightly as it neared the British Isles, skirting the coast of Western Ireland on September 16.{{Atlantic hurricane best track}} In Ireland, Debbie brought record winds to much of the island, with a peak gust of {{convert|114|mph|km/h|abbr=on}} measured just offshore.{{cite news|newspaper=Connacht Sentinel|date=September 19, 1961|title=Repairing Hurricane Damage|page=10}} {{subscription required|via=Irish Newspaper Archives}} Widespread wind damage and disruption occurred, downing tens of thousands of trees and power lines.{{cite news|newspaper=Anglo-Celt|date= September 23, 1961|title=Storm Reports From The Areas|page=9}} {{subscription required|via=Irish Newspaper Archives}}{{cite news|newspaper=Ulster Herald|date=September 23, 1961|title=The Storm Made Much Work|page=7}} {{subscription required|via=Irish Newspaper Archives}} Countless structures sustained varying degrees of damage, with many smaller buildings destroyed.{{cite journal|journal=The Irish Naturalists' Journal|author1=J. G. Gruickshank |author2=N. Stephens |author3=L. J. Symons |date=January 1962|volume=14|issue=1|pages=4–12|title=Report of the Hurricane in Ireland on Saturday, 16 September, 1961|jstor=25534822}} Agriculture experienced extensive losses to barley, corn and wheat crops.{{cite news|newspaper=Irish Farmers Journal|title=Crop Losses|date=September 23, 1961|page=1}} {{subscription required|via=Irish Newspaper Archives}} Throughout Ireland, Debbie killed 18 people, with 12 in the Republic of Ireland and six in Northern Ireland.{{cite news|newspaper=Irish Independent|date=September 18, 1961|title=Gale Killed Fifteen|page=3}} {{subscription required|via=Irish Newspaper Archives}} The storm also battered parts of Great Britain with winds in excess of {{convert|100|mph|km/h|abbr=on}}.

{{clear}}

{{Infobox Hurricane Small

| Basin = Atl

| Image = Hurricane Esther.jpg

| Track = Esther 1961 track.png

| Formed = September 10

| Dissipated = September 26

| 1-min winds = 140

| Pressure = 919

}}

{{Main|Hurricane Esther}}

On September 10, Television Infrared Observation Satellite (TIROS) III observed an area of disturbed weather well southwest of the Cape Verde Islands. Later that day, a tropical depression developed about {{convert|510|mi|km|round=5}} west-southwest of the southernmost Cape Verde Islands. Moving northwestward, the depression strengthened into Tropical Storm Esther on September 11, before reaching hurricane intensity on the following day. Early on September 13, Esther curved westward and deepened into a major hurricane. The storm remained a Category 3 hurricane for about four days and gradually moved in west-northwestward direction. Esther strengthened into a Category 4 hurricane on September 16 and peaked as a Category 5 hurricane on the following day with sustained winds of {{convert|160|mph|km/h|abbr=on|round=10}}.{{Atlantic hurricane best track}}

The storm curved north-northeastward on September 19, while offshore North Carolina. Esther began to weaken while approaching New England and fell to Category 2 intensity early on September 21. The storm turned eastward on the following day and gradually weakened to a tropical storm. It then executed a large cyclonic loop, until curving northward on September 25. Early on the following day, Esther made two landfalls in Massachusetts, first on Muskeget Island and then near South Yarmouth with winds of {{convert|60|mph|km/h|abbr=on}}. The storm then emerged over the Gulf of Maine and made landfall in Brunswick, Maine, around 11:00 UTC on September 26 with winds of {{convert|40|mph|km/h|abbr=on}}. Esther weakened to a tropical depression late on September 26 before weakening to a tropical depression and becoming extratropical over southeastern Quebec.{{Atlantic hurricane best track}} The remnants persisted for about 12 hours, before dissipating early on September 27.{{Atlantic hurricane best track}} Between North Carolina and New Jersey effects were primarily limited to strong winds and minor beach erosion and coastal flooding due to storm surge.{{cite report|url=http://docs.lib.noaa.gov/rescue/hurricanes/Qc9452e82h81961.pdf|title=Hurricane Esther — September 12–26, 1961 Preliminary Report|year=1961|work=National Weather Bureau|publisher=National Oceanic and Atmospheric Administration|page=4|access-date=March 28, 2014|location=Miami, Florida}} In New York, strong winds led to severe crop losses and over 300,000 power outages. High tides caused coastal flooding and damaged a number of pleasure boats. Similar impact was reported in Massachusetts. Additionally, some areas observed more than {{convert|8|in|mm}} of rainfall, flooding basements, low-lying roads, and underpasses. Overall, damage was minor, totaling about $6 million. There were also seven deaths reported when a United States Navy P5M aircraft crashed about {{convert|120|mi|km}} north of Bermuda.{{cite report|url=http://www.ss346.com/PDFs/ImhofRescue1961.pdf |title=Rescue at Sea |access-date=March 28, 2014 |author=Patrick J. Imhof |pages=4–6 |date=September 13, 2005 |location=Pensacola, Florida |url-status=dead |archive-url=https://web.archive.org/web/20120204203444/http://www.ss346.com/PDFs/ImhofRescue1961.pdf |archive-date=February 4, 2012 |df=mdy }}

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{{Infobox Hurricane Small

| Basin = Atl

| Image = Tropical Storm Six (1961).JPG

| Track = 1961 Atlantic tropical storm 6 track.png

| Formed = September 12

| Dissipated = September 15

| 1-min winds = 55

| Pressure = 996

}}

TIROS III imagery indicated a vortex east of the Bahamas between September 9 and September 12.{{cite report|url=https://journals.ametsoc.org/view/journals/mwre/90/8/1520-0493_1962_090_0351_ntc_2_0_co_2.xml?tab_body=pdf|title=Northbound Tropical Cyclone|author=Richard Fay|date=August 1962|publisher=National Oceanic and Atmospheric Administration|work=United States Weather Bureau|access-date=August 31, 2021}} A tropical depression formed at 12:00 UTC on September 12 near Great Harbour Cay in the Bahamas,{{Atlantic hurricane best track}} after TIROS revealed a surface circulation. The depression tracked northward and intensified into a tropical storm while located offshore North Carolina. Around 12:00 UTC September 14, it made landfall in the state near Topsail Beach, North Carolina, with winds of {{convert|45|mph|km/h|abbr=on}}. The storm curved accelerated northeastward and intensified despite mostly remaining over land, striking near the southern tip of the Delmarva Peninsula about nine hours later with winds of {{convert|50|mph|km/h|abbr=on}}. After re-emerging into the Atlantic late on September 14, the cyclone made landfall near Islip, New York, with peak winds of {{convert|65|mph|km/h|abbr=on}} around 06:00 UTC on September 15, followed by another landfall near Guilford, Connecticut, about an hour later at the same intensity. The cyclone became extratropical over southern Maine around 12:00 UTC and quickly dissipated.{{Atlantic hurricane best track}}

Impact from the storm was generally minor. In Savannah, Georgia, the storm produced an F2 tornado that blew the roof off of a lumber company building. In North Carolina, {{convert|3.12|in|mm}} of precipitation fell at Williamston.{{Tropical Cyclone Point Maxima}} Strong winds lashed Rhode Island, with winds as high as {{convert|70|mph|km/h|abbr=on}} in Point Judith. About 29,000 homes were left without electricity, while 1,200 lost telephone service. Hundreds of small crafts and a few ferries and barges were swamped or sank. Hurricane-force wind gusts in Massachusetts felled trees, electrical wires, and TV antennas. Some roads in the southeastern portion of the state were blocked by fallen trees. Similar impact was reported in Maine, where an F2 tornado/waterspout tracked {{convert|19.1|mi|km}} from Beals through Roque Bluffs before dissipating in Dog Town just east of East Machias. Power lines were considerably damaged and numerous trees were knocked down, including two incidents where trees fell on and damaged homes. The tornado caused one injury when a man was hit by a flying wooden plank.

{{clear}}

{{Infobox Hurricane Small

| Basin = Atl

| Image = Hurricane Frances analysis 9 Oct 1961.png

| Track = Frances 1961 track.png

| Formed = September 30

| Dissipated = October 9

| 1-min winds = 115

| Pressure = 948

}}

A westward-moving tropical wave organized into Tropical Storm Frances on September 30, east of the northern Lesser Antilles.{{cite report|title=Hurricane Frances, Sept. 30 – Oct. 9, 1961|url=http://atlas.amicale-des-ouragans.org/dossiers/frances1961/1961_Frances.pdf|location=Miami, Florida|work=United States Weather Bureau|publisher=National Oceanic and Atmospheric Administration|access-date=August 31, 2021|format=PDF}}{{Atlantic hurricane best track}} Six hours later, the depression strengthened into Tropical Storm Frances. Heading westward, it crossed through the Leeward Islands and entered the Caribbean Sea on October 1.{{Atlantic hurricane best track}} Thereafter, the lack of divergence at high levels prevented significant strengthening for a few days. While situated south of Puerto Rico on October 2, Frances curved northwestward.{{Atlantic hurricane best track}} The storm brought heavy rainfall to Puerto Rico, peaking at {{convert|10.15|in|mm}} in the Indiera Baja barrio of Maricao.{{Tropical Cyclone Point Maxima}} Considerable damage to roads and bridges occurred. However, due to swift evacuations of residents by the Civil Defense and American Red Cross, no fatalities were reported.

Tracking to the northwest, Frances made landfall near Punta Cana, Dominican Republic, early on October 3 with winds of {{convert|60|mph|km/h|abbr=on}}. No impact was reported on the island. Later on October 3, Frances emerged into the Atlantic Ocean just southeast of the Turks and Caicos Islands. Thereafter, the storm accelerated somewhat and resumed intensification, reaching hurricane status on October 4. Around that time, it curved northeastward and deepened further. Early on October 7, Frances attained its peak intensity with winds of {{convert|130|mph|km/h|abbr=on}} and a minimum barometric pressure of {{convert|948|mbar|inHg|abbr=on}}.{{Atlantic hurricane best track}} The storm passed by Bermuda around that time, where it dropped {{convert|1.35|in|mm}} of precipitation.{{Tropical Cyclone Point Maxima}} Later on October 7, Frances re-curved to the north. Early on the following day, the storm became extratropical as it approached the Gulf of Maine. The remnants curved east-northeastward and struck Nova Scotia, before dissipating early on October 10.{{Atlantic hurricane best track}}

{{clear}}

{{Infobox Hurricane Small

| Basin = Atl

| Track = Gerda 1961 track.png

| Image = Tropical Storm Gerda surface analysis October 20, 1961.png

| Formed = October 17

| Dissipated = October 20

| 1-min winds = 60

| Pressure = 988

}}

A westward-moving tropical wave reached the central Caribbean by mid-October. The wave crossed Jamaica, causing flooding that damaged roads and forced many to evacuate their homes in western Kingston. Five fatalities were reported in Jamaica.{{cite news|url=http://www.nhc.noaa.gov/archive/storm_wallets/atlantic/atl1961/gerda/news/savannah.gif|title=Floods Fatal To 5 Jamaicans|date=October 20, 1961|agency=Associated Press|newspaper=Savannah Morning News|page=5B|access-date=August 18, 2013|location=Kingston, Jamaica}} Early on October 17, the wave developed into a tropical depression just southwest of Cape Cruz, Cuba. It continued northward and made another landfall near Santa Cruz del Sur several hours later.{{Atlantic hurricane best track}} The depression also brought heavy rainfall to eastern Cuba, which resulted in seven deaths. After striking Cuba, the depression emerged into the Atlantic early on October 18 as it intensified into Tropical Storm Gerda.{{Atlantic hurricane best track}}

Moving across the Bahamas later on October 18, Gerda accelerated to the north-northeast. The storm curved northeastward on October 20, while peaking with winds of {{convert|70|mph|km/h|abbr=on}}.{{Atlantic hurricane best track}} However, a Texas Tower offshore Massachusetts observed hurricane-force winds. At 00:00 UTC on October 20, Gerda transitioned into an extratropical cyclone while situated about {{convert|165|mi|km|round=5}} southeast of Nantucket, Massachusetts.{{Atlantic hurricane best track}} Damage from the storm in New England was "about the same as that from a typical wintertime northeaster". The remnants of Gerda moved northeastward and then to the east, before dissipating between Newfoundland and the Azores late on October 22.{{Atlantic hurricane best track}}

{{clear}}

{{Infobox Hurricane Small

| Basin = Atl

| Image = Hurricane Hattie radar 30 Oct 1961 - cropped.jpg

| Track = Hattie 1961 track.png

| Formed = October 27

| Dissipated = November 1

| 1-min winds = 145

| Pressure = 914

}}

{{Main|Hurricane Hattie}}

In late October, an area of low pressure persisted in the western Caribbean Sea for several days.{{cite report|url=http://docs.lib.noaa.gov/rescue/hurricanes/Qc9452h39h81961.pdf|title=Hurricane Esther — October 27–31, 1961 Preliminary Report|year=1961|work=National Weather Bureau|publisher=National Oceanic and Atmospheric Administration|page=4|access-date=August 31, 2021|location=Miami, Florida|archive-url=https://web.archive.org/web/20170429192329/http://docs.lib.noaa.gov/rescue/hurricanes/Qc9452h39h81961.pdf|archive-date=April 29, 2017}} Around 00:00 UTC on October 26, a tropical depression developed about {{convert|100|mi|km|abbr=on|round=5}} northeast of Colón, Panama. Approximately 12 hours later, the depression intensified into Tropical Storm Hattie. Moving towards the north and north-northeast, the storm quickly gained hurricane status early on October 28 and reached major hurricane intensity that same day. Hattie turned towards the west to the east of Jamaica and strengthened into a Category 5 hurricane with maximum sustained winds of {{convert|165|mph|km/h|abbr=on}} on October 31. The storm then weakened to a Category 4 hurricane prior to landfall south of Belize City, British Honduras, with winds of {{convert|150|mph|km/h|abbr=on}}. Continuing southwest, the storm rapidly weakened over the mountainous terrain of Central America, dissipating on November 1.{{Atlantic hurricane best track}} It was originally thought that the remnants may have contributed to the development of Tropical Storm Simone in the eastern Pacific Ocean, but a 2019 reanalysis concluded that the remnants of Hattie instead became a Central American gyre.

Hattie first affected regions in the southwestern Caribbean, producing hurricane-force winds and causing one death on San Andres Island. It was initially forecast to continue north and strike Cuba, which prompted evacuations.{{cite news|title='Cane Hattie Threatens Western Cuba, Florida|agency=Associated Press|newspaper=The Palm Beach Post|page=1|location=West Palm Beach, Florida|date=October 30, 1961|access-date=February 6, 2021|url=https://www.newspapers.com/clip/46430170/the-palm-beach-post/|via=Newspapers.com}} {{free access}} Little effects were reported as Hattie turned to the west, although rainfall reached {{convert|11.5|in|mm|abbr=on}} on Grand Cayman. The worst damage was in the country of Belize. The former capital, Belize City, was flooded by a powerful storm surge and high waves and affected by strong winds. The territory governor estimated 70% of the buildings in the city were damaged, which left over 10,000 people homeless.{{cite news|agency=United Press International|date=November 2, 1961|title=Hattie's Toll is 62: Martial Law Declared|newspaper=St. Petersburg Times|pages=1A, 2A|location=St. Petersburg, Florida|access-date=March 28, 2014|url=https://news.google.com/newspapers?id=204nAAAAIBAJ&sjid=JHkDAAAAIBAJ&pg=5523%2C397222}} The damage was severe enough that it prompted the government to relocate inland to a new city, Belmopan.{{cite news|newspaper=Sarasota Herald-Tribune|date=September 7, 1971|title=Hurricane 'Edith' Deepens Rapidly|agency=Associated Press|pages=1A, 4A|location=Sarasota, Florida|access-date=March 28, 2014|url=https://news.google.com/newspapers?id=HjogAAAAIBAJ&sjid=c2YEAAAAIBAJ&pg=7339,2936965}} In the territory, Hattie left about $60 million in damage and caused 307 deaths.{{cite press release|title=Belize Marked 45th Anniversary of Deadly Hurricane Hattie |url=http://www.nemo.org.bz/cgi-bin/nemonews/exec/view.cgi?archive=1&num=285 |work=Belize National Emergency Management Organization (NEMO) |access-date=December 3, 2012 |publisher=NEMO Press Officer |archive-url=https://web.archive.org/web/20120723114312/http://www.nemo.org.bz/cgi-bin/nemonews/exec/view.cgi?archive=1&num=285 |archive-date=July 23, 2012 |date=November 2, 2006 |url-status=dead }} The government estimated that Hattie was more damaging than a hurricane in 1931 that killed 2,000 people; the lower toll for Hattie was due to advance warning. Elsewhere in Central America, the hurricane killed 11 people in Guatemala and one in Honduras.

{{clear}}

{{Infobox Hurricane Small

| Basin = Atl

| Track = Jenny 1961 track.png

| Image = Hurricane Jenny surface analysis November 6, 1961.png

| Formed = November 1

| Dissipated = November 10

| 1-min winds = 70

| Pressure = 974

}}

A surface trough of low pressure developed in the eastern Caribbean Sea on October 30. The trough split, with the northern portion spawning a tropical depression near Antigua at 00:00 UTC on November 2.{{Atlantic hurricane best track}}{{cite report|author=David M. Roth|work=Weather Prediction Center|publisher=National Oceanic and Atmospheric Administration|date=October 16, 2008|access-date=March 28, 2014|title=Hurricane Jenny – October 30 November 2, 1961|url=http://www.wpc.ncep.noaa.gov/tropical/rain/jenny1961.html|location=College Park, Maryland}} The precursor to Jenny brought light rainfall to Puerto Rico, peaking at {{convert|4.97|in|mm}} in Río Blanco, Naguabo. Moving northeastward ahead of an upper-level trough, the depression remained weak for over three days. On November 3, the system curved eastward, before briefly turning to the southeast on November 4. The depression tracked in a circular path during the next 24 hours, moving northeastward, north-northwestward, and then west-northward. Finally, the system strengthened into Tropical Storm Jenny early on November 5.{{Atlantic hurricane best track}}

Jenny intensified further and reached hurricane status at 12:00 UTC on November 6. Later that day, the United States Weather Bureau began advisories and described Jenny as having "characteristic of many storms in the sub-tropics late in the hurricane season."{{cite report|title=Hurricane Jenny, November 6-8, 1961|url=http://docs.lib.noaa.gov/rescue/hurricanes/Qc9452j45h81961.pdf|location=Miami, Florida|work=United States Weather Bureau|publisher=National Oceanic and Atmospheric Administration|access-date=March 28, 2014}} Around 18:00 UTC on November 6, Jenny attained its peak intensity with maximum sustained winds of {{convert|80|mph|km/h|abbr=on}} and a minimum barometric pressure of {{convert|974|mbar|inHg|abbr=on}}. Thereafter, the storm briefly decelerated and weakened, falling to tropical storm intensity around midday on November 7. Jenny curved northeastward and continued to weaken, transitioning into an extratropical cyclone late on November 10 about {{convert|545|mi|km|abbr=on|round=5}} east of Cape Race, Newfoundland.{{Atlantic hurricane best track}} The extratropical remnants continued to move northeastward and weakened before being absorbed by a larger extratropical cyclone on the following day.{{rp|97}}

{{clear}}

{{Infobox Hurricane Small

| Basin = Atl

| Image = Tropical Storm Inga analysis 6 Nov 1961.png

| Track = Inga 1961 track.png

| Formed = November 4

| Dissipated = November 8

| 1-min winds = 60

| Pressure = 997

}}

Early on November 4, the SS Navigator encountered a weather system in the Gulf of Mexico that produced northwesterly winds of {{convert|81|to|92|mph|km/h|abbr=on}}. Reconnaissance aircraft data indicated that Tropical Storm Inga developed at 00:00 UTC on November 4, while located about {{convert|145|mi|km|round=5}} northeast of Veracruz.{{Atlantic hurricane best track}} A strong high pressure system and a cold front entering the Gulf of Mexico from Texas caused the storm to move southward and then southeastward. Inga slowly strengthened and peaked as a {{convert|70|mph|km/h|abbr=on}} tropical storm early on November 7. Thereafter, the storm became nearly stationary and began weakening. By 12:00 UTC on November 8, Inga dissipated in the Bay of Campeche,{{Atlantic hurricane best track}} as reconnaissance aircraft found no closed circulation.

{{clear}}

{{Infobox Hurricane Small

| Basin = Atl

| Image =

| Track = 1961 Atlantic tropical storm 12 track.png

| Formed = November 17

| Dissipated = November 20

| 1-min winds = 50

| Prepressure = ≤

| Pressure = 992

}}

A stationary front across the central Atlantic Ocean led to the development of a low pressure area by November 16, northeast of the Lesser Antilles. A day later, it is estimated that a tropical depression developed, although due to the system's large size, it was possible it was a subtropical cyclone. The depression moved northeastward and slowly intensified, based on observations from nearby ships. On November 19, the depression strengthened into a tropical storm. The storm strengthened to reach peak winds of {{convert|60|mph|km/h|abbr=on}} on November 20. By that time, a cold front was approaching the storm, causing the storm to transition into an extratropical cyclone on November 21; later that day, the front absorbed the former tropical storm.

{{clear}}

In addition to the twelve systems reaching at least tropical storm status, two other cyclones formed but remained at tropical depression intensity. The first such system, also the first tropical cyclone of the season, originated from a tropical wave about {{convert|35|mi|km|abbr=on|round=5}} east of Palm Bay, Florida, on June 10. Moving quickly northeastward, the depression may have reached tropical storm intensity on June 12 but degenerated into a trough offshore New England on the next day.{{rp|108}} On October 12, a trough developed into a tropical depression about halfway between Bermuda and North Carolina. This depression also moved quickly northeastward and merged with a frontal boundary by October 15.{{rp|109}}

A report from Mexico indicates that a tropical depression formed off the west coasts of Tabasco and Coatzacoalcos. The depression significantly impacted the northern portions of Veracruz with heavy rainfall on June 30.{{cite report|language=es|url=http://www.uv.mx/eventos/inundaciones2005/PDF/20_%20RIESGO.pdf|journal=Inundaciones 2005 en el Estado de Veracruz|title=Riesgo Quimico Asociado a Fenominos Hidrometeorologicos en el Estado de Verzacruz|author1=Humberto Bravo Alavarez |author2=Rodolfo Sosa Echeverria |author3=Pablo Sanchez Alavarez |author4=Arturo Butron Silva |page=317|date=June 22, 2006|publisher=Universidad Veracruzana|access-date=March 28, 2014}} However, the Atlantic hurricane best track does not list this system as a tropical depression.

The following list of names was used for named storms (tropical storms and hurricanes) that formed in the North Atlantic in 1961.{{cite news|url=https://www.newspapers.com/clip/69488210/the-miami-news/|title=Go Blame An Ill Wind|date=June 9, 1961|newspaper=The Miami News|page=1|access-date=February 6, 2021|via=Newspapers.com}} {{free access}} Storms were named Frances, Hattie, Inga and Jenny for the first time in 1961.

{{See also|List of retired Atlantic hurricane names}}

The names Carla and Hattie were retired after the season due to their severity of impacts.{{cite web|url=https://www.nhc.noaa.gov/aboutnames_history.shtml|title=Tropical Cyclone Naming History and Retired Names|publisher=National Hurricane Center|location=Miami, Florida|access-date=February 16, 2024}} They were replaced with Carol and Holly, respectively, for the 1965 season.{{cite news|url=https://news.google.com/newspapers?id=cjBAAAAAIBAJ&sjid=ClkMAAAAIBAJ&pg=771,2204280&dq=hurricane+anna+betsy+carol&hl=en|title="Anna" Will Be First Hurricane|date=May 23, 1965|agency=Associated Press|newspaper=Youngstown Vindicator|page=2|access-date=February 20, 2013}}

This is a table of all of the storms that formed in the 1961 Atlantic hurricane season. It includes their name, duration, peak classification and intensities, areas affected, damage, and death totals. Deaths in parentheses are additional and indirect (an example of an indirect death would be a traffic accident), but were still related to that storm. Damage and deaths include totals while the storm was extratropical, a wave, or a low, and all of the damage figures are in 1961 USD.

{{Saffir-Simpson small|align=center}}

{{Portal|Tropical cyclones}}

• 1961 Pacific hurricane season
• 1961 Pacific typhoon season
• 1961 North Indian Ocean cyclone season
• Australian region cyclone seasons: 1960–61 1961–62
• South Pacific cyclone seasons: 1960–61 1961–62
• South-West Indian Ocean cyclone seasons: 1960–61 1961–62

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• [http://www.aoml.noaa.gov/general/lib/lib1/nhclib/mwreviews/1961.pdf Monthly Weather Review]

{{Highest ACE Atlantic hurricane seasons navbox}}

{{1961 Atlantic hurricane season buttons}}

{{TC Decades|Year=1960|basin=Atlantic|type=hurricane}}

{{Tropical cyclone season|1961}}

Category:Articles which contain graphical timelines