• No results found

CPC Monthly Climate Review

N/A
N/A
Protected

Academic year: 2022

Share "CPC Monthly Climate Review"

Copied!
59
0
0

Bezig met laden.... (Bekijk nu de volledige tekst)

Hele tekst

(1)

CPC Monthly Climate Review

September 2014

Yan Xue Outline:

1. Global Patterns

2. Tropical Climate Variability

ENSO, MJO, IOD, TAV, Hurricane Season 3. Extra-Tropical Climate Variability

PDO, NAO, Asia and N. America Monsoons, Ozone Hole

4. U.S. Climate, Outlooks and Verifications

Thanks to Anthony Artusa, Mingyue Chen/Wanqiu Wang, Wei Shi, Kingtse Mo, Craig Long,

Pingping Xie, Muthu Chelliah, Caihong Wen, Michelle L’Heureux, Jon Gottschalck, Jae Schemm

(2)

1. Global Patterns

(3)

SST Anomaly (

0

C) and Anomaly Tendency

http://www.cpc.ncep.noaa.gov/products/GODAS/ocean_briefing.shtml DMI= -0.5

PDO= +0.74

ENSO-neutral NINO3.4=+0.47 MDR near-normal

cooling

(4)

Upper 300m Heat Content Anomaly (

0

C) and Anomaly Tendency

http://www.cpc.ncep.noaa.gov/products/GODAS/multiora_body.html -DMI

Not clear +PDO pattern

Favourable for El Nino

(5)

N. Atlantic below-normal Unfavourable for hurricane E. Pac. above-normal

favourable for hurricane

(6)

Longitude-Depth Temperature Anomaly and Anomaly Tendency in 1

O

S-1

O

N

http://www.cpc.ncep.noaa.gov/products/GODAS/multiora_body.html

(7)

Sea Surface Salinity (SSS) and E-P Anomaly

From Pingping Xie enhanced

precipitation

enhanced

precipitation

(8)

ENSO

2. Tropical Climate Variability

(9)

SST Indices

(10)

SOI < 0: El Nino-Like

OLR < 0: El Nino-Like OLR > 0: La Nina-Like u850 < 0: El Nino favorable

u850 > 0: La Nina favorable

SOI, Winds and OLR Indices

(11)

Weekly ENSO Update

http://www.cpc.ncep.noaa.gov/products/pr

ecip/CWlink/MJO/enso.shtml

(12)

Depth of 20C Isotherm Anomaly (2S-2N, GODAS)

850mb Zonal Wind Anomaly

(5S-5N, NCEP R1)

(13)

SST Anomaly (2S-2N)

Sea Surface Salinity Anomaly

(5S-5N)

(14)

Tropical Pacific

Observing System

(15)

Real-Time Multiple Ocean Reanalysis Intercomparison

(http://www.cpc.ncep.noaa.gov/products/GODAS/multiora_body.html)

(16)

Upper 300m Heat Content Anomaly (1981-2010 Clim.)

(17)

Warm Water Volume Index Derived

From Ensemble Mean of Ocean Reanalyses

- Warm Water Volume averaged in Aug-Sep 2014 is similar to that in Aug-Sep of 1991, 2004, 2006, 2009.

AS 82 AS 97 AS 14

AS 02

AS 91 AS 06 AS 09

AS 86

AS 04

(18)

86/87 91/92 94/95

06/07 09/10

Upper 300m Heat Content Anomaly Averaged in 1S-1N

12/13 14/15

04/05

(19)

19

(20)
(21)

NINO3.4 Forecast Plums

(22)

MJO

2. Tropical Climate Variability

(23)

OLR Anomalies – Past 30 days

Drier-than-normal conditions, positive OLR anomalies (yellow/red shading) Wetter-than-normal conditions, negative

OLR anomalies (blue shading)

From late August to early September, enhanced (suppressed) convection was observed near India and Central America (equatorial Indian Ocean).

During mid-September, enhanced

convection was located over Southeast Asia and Central America, while the area of suppressed convection expanded near the Date Line.

During mid-September, monsoon flow over the Bay of Bengal and Southeast Asia

waned. Anomalous convection over Central America shifted northward with some areas of suppressed convection evident over the eastern Pacific.

(24)

Outgoing Longwave Radiation (OLR) Anomalies (2.5°N-17.5°N)

Drier-than-normal conditions, positive OLR anomalies (yellow/red shading)

Wetter-than-normal conditions, negative OLR anomalies (blue shading)

(Courtesy of CAWCR Australia Bureau of Meteorology)

Time

Longitude

Since April, enhanced convection has propagated slowly eastward from the Maritime Continent to the central Pacific (red box).

The MJO became more coherent during April, with the subseasonal envelopes of enhanced and suppressed convection modulating the strength of the low frequency signal. The anomalous tropical convection pattern became largely incoherent during mid-May. During June, the MJO became more organized, primarily over the Indian Ocean, but the pattern became less coherent with respect to canonical MJO activity through August.

There is evidence of westward-moving subseasonal variability from mid-August and later. Recently, anomalous convection has increased near 150E while waning over the eastern Pacific.

(25)

200-hPa Velocity Potential Anomalies (5°S-5°N)

Positive anomalies (brown shading) indicate unfavorable conditions for precipitation Negative anomalies (green shading) indicate favorable conditions for precipitation

Time

Longitude

A slow eastward progression of negative anomalies was observed from March to present across the Indo-Pacific warm pool and central Pacific (red box).

During March through April, anomalies

propagated eastward with time associated with the MJO before weakening for much of May.

The pattern became more organized during June with a more coherent wave-1 MJO-like structure with eastward propagation.

The pattern became less coherent during early July, but then organized again in late July and August, with a wide area of suppressed convection moving around the planet.

During mid-September, anomalies were generally small with positive (negative) anomalies over the eastern Pacific (over the Indian Ocean and near 150E).

(26)

IOD, TAV, Hurricane

2. Tropical Climate Variability

(27)

Evolution of Indian Ocean SST Indices

Fig. I1a. Indian Ocean Dipole region indices, calculated as the area-averaged monthly mean sea surface temperature anomalies (OC) for the SETIO [90ºE-110ºE, 10ºS-0] and WTIO [50ºE-70ºE, 10ºS-10ºN]

regions, and Dipole Mode Index, defined as differences between WTIO and SETIO. Data are derived from the NCEP OI SST analysis, and anomalies are departures from the 1981-2010 base period means.

- Negative DMI persisted in September.

(28)

Evolution of Tropical Atlantic SST Indices

Fig. A1a. Tropical Atlantic Variability region indices, calculated as the area-averaged monthly mean sea surface temperature anomalies (ºC) for the TNA [60ºW-30ºW, 5ºN-20ºN], TSA [30ºW-10ºE, 20ºS-0] and ATL3 [20ºW-0, 2.5ºS-2.5ºN] regions, and Meridional Gradient Index, defined as differences between TNA and TSA. Data are derived from the NCEP OI SST analysis, and anomalies are departures from the 1981-2010 base period means.

-TNA – TSA gradient index has been below-normal since Feb 2014, unfavourable for hurricane activity.

(29)

2014 Atlantic Hurricane Counts

(http://weather.unisys.com/hurricane)

- Atlantic Outlook (Aug update, 70% above-normal):

7-12 Named Storms (12 average) 3-6 Hurricanes (6 average)

0-2 Major Hurricanes (3 average) 40%-90% ACE

- Atlantic Counts by Oct 6:

5 Named Storms 4 Hurricanes

1 Major Hurricanes 41% ACE

- Only three seasons since 1995 were below normal (1997, 2009, and 2013).

- If the current outlook verifies, 2014 will become the fourth below-normal season since 1995.

- It would mark the first

time since 1995 that two

consecutive seasons

were below-normal.

(30)
(31)
(32)
(33)

- E. Pacific Counts by Oct 6:

19 Named Storms 14 Hurricanes

5 Major Hurricanes 142% ACE

2014 E. Pacific Hurricane Counts

(http://weather.unisys.com/hurricane)

- E. Pacific Outlook (50% above-normal):

14-20 Named Storms (15 average)

7-11 Hurricanes (8 average)

3-6 Major Hurricanes (4 average) 95%-160% ACE

(34)

Last Three Month SST, OLR and 925hp Wind Anom.

(35)

3. Extra-Tropical Climate Variability

PDO, NAO, Monsoons, Ozone Hole,

(36)

PDO index

- Pacific Decadal Oscillation is defined as the 1st EOF of monthly ERSST v3b in the North Pacific for the period 1900- 1993. PDO index is the standardized projection of the monthly SST anomalies onto the 1st EOF pattern.

- The PDO index differs slightly from that of JISAO, which uses a blend of UKMET and OIv1 and OIv2 SST.

- PDO index enhanced in Sep with PDO index

=+0.74

(37)

NAO and SST Anomaly in North Atlantic

Fig. NA2. Monthly standardized NAO index (top) derived from monthly standardized 500-mb height anomalies obtained from the NCEP CDAS in 20ºN-90ºN (http://www.cpc.ncep.noaa.gov). Time-Latitude section of SST anomalies averaged between 80ºW and 20ºW (bottom). SST are derived from the NCEP OI SST analysis, and anomalies are departures from the 1981-2010 base period means.

- NAO index switched to a strong positive phase , with NAO index= in September 2014.

- Large positive SST anomaly presented near the east coast of Canada and Norwegian Sea.

- High-latitude North Atlantic SSTA are reversely related to NAO index (negative NAO coincides with SST warming).

(38)

Rainfall Anomaly Patterns

Hurricane Odile (Sept 10-17) contributed significant rainfall to Southwest US and Northwest Mexico in September.

Overall for the NAM region during JAS: near to above-average in the northern part but dry in the south.

September 2014 JAS 2014

From Wei Shi

(39)

Seasonal Evolution: Rainfall

From Wei Shi

Category 4 hurricane Odile

(40)

India Met. Dept. (IMD) Forecast:

Rainfall over the country as a whole for the 2014 southwest monsoon season (June-September)

is likely to be below normal (90-96%

of normal).

OBSERVED: INDIA 2014 SUMMER MONSOON SEASON (1 June – 30 September) 12% BELOW NORMAL

From Muthu

(41)

From Craig

(42)

4. U.S. Climate (drought),

Outlooks and Verifications

(43)

U.S. Temperature and Precipitation Departures During U.S. Temperature and Precipitation Departures During

the Last 30 Days the Last 30 Days

End Date: 27 September 2014

Percent of Average

Precipitation Temperature Departures

(degree C)

1 of 2

(44)

SST along N. America Coast

(45)

DROUGHT MONITOR

S LS LS LS S S LLLS LS LS LS S S S LS S S S S S S S S S S LS LS LS LS S LLS LS LS LS S S S LS S S S S S S S S S S S S L

T heD roughtM onitorfocusesonbroad-scaleconditions.Localconditionsm ayvary.S eeaccom panyingtextsum m aryforforecaststatem ents.

L h ttp ://d rough tm on ito r.un l.edu

/ U

.S .D roughtM onito r

Ju ly29 ,2014

V alid8a.m .E D T (R eleasedT hursday,Jul.31,2014)Intensity:

D 0A bnorm allyD ryD 1M oderateD roughtD 2S evereD roughtD 3E xtrem eD roughtD 4E xceptionalD rought

A uthor:B radR ippeyD roughtIm pactT ypes:

S

= S hort-T erm ,typicallylessthan6m onths(e.g.agriculture,grasslands)L=

Long-T erm ,typicallygreaterthan6m onths(e.g.hydrology,ecology)D elineatesdom inantim pacts

U .S .D epartm entofA gricultur e

- Low water levels are visible

at the Almaden Reservoir on

January 28, 2014 in San

Jose, Calif.

(46)

46

Streamflow Percentiles (USGS)

Dryness: California, Texas

Texas drought improved

Wetness: Dakotas , Minn, Wisconsin, Missouri basin, Great Lakes

July 2014 AUG

Sep

From Kingtse Mo

(47)

California Reservoir Conditions

47

Most reservoirs are only 11-30% capacity

From Kingtse Mo

(48)

Oct 2014 Outlook

(49)

OND 2014 Outlook

(50)
(51)
(52)
(53)
(54)

Thanks!

(55)

Global Temperatures

(56)

Global Precipitation

(57)

U.S. Temperature and Precipitation Departures During the U.S. Temperature and Precipitation Departures During the

Last 30 Days Last 30 Days

End Date: 4 October 2014

Percent of Average

Precipitation Temperature Departures

(degree C)

1 of 2

(58)

U.S. Temperature and Precipitation Departures During the U.S. Temperature and Precipitation Departures During the

Last 90 Days Last 90 Days

End Date: 4 October 2014

Percent of Average

Precipitation Temperature Departures

(degree C)

2 of 2

(59)

Monsoon precip

59

Very good monsoon relieved drought

90day % of normal

P anomalies (90 day mean)

Referenties

GERELATEERDE DOCUMENTEN

- Large positive SW+LW anomalies were observed in the Artic Ocean and the high latitudes of North Pacific, leading to. significant warming in

During late June and early July, enhanced (suppressed) convection was observed over both the western and eastern Pacific.. (northern Indian Ocean and parts of

During early June, a more coherent pattern of enhanced (suppressed) convection developed over the Indian Ocean, Maritime Continent, and Australia (central and eastern Pacific

- Positive SSTA was observed in the Indian Ocean and western Pacific.. - Above-normal SST occurred in high and low latitudes of

Anomalies (5°S-5°N) Positive anomalies (brown shading) indicate unfavorable conditions for precipitation Negative anomalies (green shading) indicate favorable conditions

During March and early April, anomalies indicate signs of being influenced by equatorial Rossby wave activity with less eastward propagation evident. The MJO strengthened

Thanks to Scott Handel for pointing me to high-resolution satellite imagery at the:. NOAA Environmental Visualization

Eastward propagation was evident from late May into September associated with the MJO (alternating dashed and dotted lines), as well as atmospheric Kelvin wave activity, which at