CPC Monthly Climate Review
August 2014
Yan Xue Outline:
1. Global Patterns
2. Tropical Climate Variability
ENSO, MJO, IOD, TAV, Hurricane Season 3. Extra-Tropical Climate Variability
PDO, NAO, Ozone Hole, Monsoon
1. U.S. Climate, Outlooks and Verifications
Thanks to Anthony Artusa, Mingyue Chen/Wanqiu Wang, Craig Long, Pingping Xie, Muthu Chelliah,
Caihong Wen, Matthew Rosencrans, Michelle L’Heureux, Jon Gottschalck, Wei Shi, Scott Weaver
1. Global Patterns
SST Anomaly ( 0 C) and Anomaly Tendency
http://www.cpc.ncep.noaa.gov/products/GODAS/ocean_briefing.shtml DMI= -0.7
PDO= +0.3
ENSO-neutral
MDR below-normal
Upper 300m Heat Content Anomaly (
0C) and Anomaly Tendency
http://www.cpc.ncep.noaa.gov/products/GODAS/multiora_body.html -DMI
PDO?
Favourable for El Nino
N. Atlantic below-normal Unfavourable for hurricane
E. Pac. above-normal
favourable for hurricane
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
OLR and 850mb Wind Anomalies
Sea Surface Salinity (SSS) and E-P Anomaly
From Pingping Xie suppressed
precipitation
enhanced
precipitation
ENSO
2. Tropical Climate Variability
SST Indices
SOI < 0: El Nino-Like SOI > 0: La Nina-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
Weekly ENSO Update
http://www.cpc.ncep.noaa.gov/products/pr
ecip/CWlink/MJO/enso.shtml
Depth of 20C Isotherm Anomaly (2S-2N, GODAS)
850mb Zonal Wind Anomaly
(5S-5N, NCEP R1)
Tropical Pacific Observing System
Real-Time Multiple Ocean Reanalysis Intercomparison
(http://www.cpc.ncep.noaa.gov/products/GODAS/multiora_body.html)
Upper 300m Heat Content Anomaly (1981-2010 Clim.)
Warm Water Volume Index Derived
From Ensemble Mean of Ocean Reanalyses
- Warm Water Volume averaged in Jul-Aug 2014 is similar to that in Jul-Aug of 2004, 2006, 2009 and 2012.
JA 82 JA 97
JA 14 JA 02
JA 91 JA 06 JA 09
JA 86
JA 04 JA 12
Aug 2004
(DJF NINO3.4=+0.6)
Aug 2014 Aug 2006
(DJF NINO3.4=+0.7) Aug 2009
(DJF NINO3.4=+1.6)
Aug 2012
(DJF NINO3.4=-0.6)
86/87 02/03 04/05
06/07 09/10
Upper 300m Heat Content Anomaly Averaged in 5S-5N
12/13 14/15
14/15
20
21
too warm forecast Good forecast
22
NINO3.4 Forecast Plums
MJO
2. Tropical Climate Variability
850-hPa Vector Wind Anomalies (m s -1 )
Note that shading denotes the zonal wind anomaly
Blue shades: Easterly anomalies
Red shades: Westerly anomalies
Westerly anomalies increased over Africa and persisted over the tropical Atlantic.
Westerly anomalies increased north of the equator over the eastern Pacific, with weak anomalies on the equator.
Monsoon flow increased over South Asia.
Weak easterly anomalies
spread across the west-
central Pacific.
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 January to present across the Indo-Pacific warm pool and central Pacific (red box).
During February 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 July and August as other modes of subseasonal tropical variability, e.g., equatorial Rossby and Kelvin wave activity, became the more dominant signals.
More recently, the signal strengthened with some
eastward propagation.
CFSv2 Precipitation Forecast
CFSv2 850mb Wind Forecast
IOD, TAV, Hurricane
2. Tropical Climate Variability
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 enhanced in August.
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.
- Tropical North Atlantic (TNA) index was negative since Jan 2014.
- Tropical South Atlantic (TSA) index continued to be near-normal .
- Meridional Gradient Mode (TNA-TSA) remained negative.
- Negative ATL3 SSTA strengthened in Aug. 2014.
2014 Atlantic Hurricane Counts
(http://weather.unisys.com/hurricane)
- Atlantic Outlook (Aug update):
7-12 Named Storms (12 average) 3-6 Hurricanes (6 average)
0-2 Major Hurricanes (3 average)
- E. Pacific Counts by Sep 6:
15 Named Storms 3 Hurricanes
7 Major Hurricanes
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)
# Name Date Win
d Pres Cat 1 Hurricane-4 AMANDA 22-29 MAY 135 4 2 Tropical Storm BORIS 02-04 JUN 35 - 3 Hurricane-4 CRISTINA 09-15 JUN 130 4 4 Tropical Storm DOUGLAS 28 JUN-05 JUL 40 - 5 Tropical Storm ELIDA 30 JUN-02 JUL 45 - 6 Tropical Storm FAUSTO 07-09 JUL 40 - 7 Tropical Storm WALI 17-19 JUL 40 - 8 Hurricane-5 GENEVIEVE 25 JUL-11 AUG 140 5 9 Hurricane-1 HERNAN 26-29 JUL 65 1 10 Hurricane-4 ISELLE 31 JUL-09 AUG 120 4 11 Hurricane-3 JULIO 04-15 AUG 105 3 12 Hurricane-1 KARINA 13-27 AUG 70 1 13 Hurricane-1 LOWELL 18-24 AUG 65 1 14 Hurricane-5 MARIE 22-29 AUG 140 5
15 Hurricane-3 NORBERT 02-07 SEP 105 3 Active
The strongest tropical cyclone ever recorded in May
the strongest tropical cyclone on record to strike the Big Island of Hawaii
3. Extra-Tropical Climate Variability
PDO, NAO, Ozone Hole, Monsoon
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 has been in positive
phase since Mar 2014, and PDO
index = +0.3 in August 2014.
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 was well below-normal , with NAO= -2.3 in August 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
to SST warming).
From Craig Long
The black line highlights the -78C isotherm.
Temps colder than -78C are required to form
polar stratospheric clouds upon which solar
driven ozone depletion occurs.
• India 2104 summer monsoon rainfall, so far this season (since 1
stJune) is about 11% BELOW normal. This is much
improved compared to about 45% below normal earlier in the season.
Recent Heavy rains, Floods and mudslides in northern India in
Kashmir region. (1-7 Sep.
2014).
Forecast anom Observed anom
From Muthu Chelliah
4. U.S. Climate, Outlooks and Verifications
U.S. Temperature and Precipitation Departures During U.S. Temperature and Precipitation Departures During
the Last 30 Days the Last 30 Days
End Date: 31 August 2014
Percent of Average Precipitation
Temperature Departures
(degree C)
1 of
2
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 heDroughtM onitorfocusesonbroad-scaleconditions.L ocalconditionsm ayvary.S eeaccom panyingtextsum m aryforforecaststatem ents.
L h ttp ://d rough tm on ito r.un l.edu/
U .S .D roughtM onitor
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 ippey D roughtIm pactTy pes:
S
= S hort-T erm ,typicallylessthan6m onths(e.g.agriculture,grasslands)L
= L ong-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.
AUG TEMP AUG PRCP
Sept 2014 Outlook
SON 2014 Outlook
Thanks!
Global Temperatures
Global Precipitation
U.S. Temperature and Precipitation Departures During the U.S. Temperature and Precipitation Departures During the
Last 90 Days Last 90 Days
End Date: 31 August 2014
Percent of Average
Precipitation Temperature Departures
(degree C)
2 of
2
Mar 1
Apr 1
May 1
Jun 1
Jul 1
Aug 1
Aug 2004
(DJF NINO3.4=+0.6)
Aug 2014 Jul 2006
(DJF NINO3.4=+0.7) Jul 2009
(DJF NINO3.4=+1.6)
Aug 2012 (DJF NINO3.4=-0.6)
5S-5N Average
58