ISRN Astronomy and AstrophysicsVolume 2013 (2013), Article ID 129426, 13 pageshttp://dx.doi.org/10.1155/2013/129426

Research Article

A Statistical Study on DH CMEs and Its Geoeffectiveness

V. Vasanth and S. Umapathy

School of Physics, Madurai Kamaraj University, Madurai 625021, India

Received 31 October 2013; Accepted 19 November 2013

Academic Editors: S. Koutchmy and Y.-D. Park

Copyright © 2013 V. Vasanth and S. Umapathy. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

Abstract.

A detailed investigation on geoeffectiveness of CMEs associated with DH-type-II bursts observed during 1997–2008 is presented. The collected sample events are divided into two groups based on their association with CMEs related to geomagnetic storms Dst ≤−50 nT, namely, (i) geoeffective events and (ii) nongeoeffective events. We found that the geoeffective events have high starting frequency, low ending frequency, long duration, wider bandwidth, energetic flares, and CMEs than nongeoeffective events. The geoeffective events are found to have intense geomagnetic storm with mean Dst index (−150 nT). There exists good correlation between the properties of CMEs and flares for geoeffective events, while no clear correlation exists for nongeoeffective events. There exists a weak correlation for geoeffective events between (i) CME speed and Dst index and good correlation between (i) CME speed and solar wind speed , (ii) Dst index and solar wind speed , and (iii) Dst index and southward magnetic field component () . From our study we conclude that the intense and long duration southward magnetic field component () and fast solar wind speed are responsible for geomagnetic storms, and the geomagnetic storms weakly depend on CME speed. About 22% (50/230) of the DH-type-II bursts are associated with geomagnetic storms. Therefore the DH-type-II bursts associated with energetic flares and CMEs are good indicator of geomagnetic storms.

1. Introduction

CMEs are large scale plasma and magnetic field structure moving away from the sun into heliosphere. If the ejected CMEs appear to surround the occulting disk they are called halo CMEs [1]. The halo CMEs that appear on the visible disk are considered to be Earth-directed and cause disturbance to our Earth’s magnetic field. The counterparts of CMEs in the interplanetary medium are called interplanetary CMEs (ICMEs), which are geoeffective because of the enhanced interplanetary magnetic field compressed by CME-driven shocks or by CMEs with strong magnetic field [2] and also due to the enhanced southward magnetic field component () along the Sun-Earth direction in the interplanetary medium. The major geomagnetic storms are mainly caused by CMEs [3–5]. The geoeffectiveness of halo CMEs was established in earlier reports [6, 7] which showed that the halo CMEs are very much effective in producing geomagnetic storms. The statistical studies have found that the earth directed CMEs will reach earth within 1–5 days depending on the CME’s initial speed [8, 9]. Richardson et al. [10] investigated the geomagnetic storms with CMEs and concluded that the intense storms are produced by CMEs at any time in the solar cycle. The CMEs that are faster and wider are more energetic and can generate shocks in the interplanetary medium [11]. The type-II bursts are the earliest signature of shocks propagating outward in the solar corona. It is now well accepted that the DH-type-II bursts are produced by CME driven shocks [9, 12]. Gopalswamy et al. [11] suggested that DH-type-II bursts are associated with more energetic CMEs, and these CMEs are good indicator of geoeffectiveness if they appear on the front side of the solar disk. In the present paper we investigate the relationship between flares and CMEs associated with DH-type-II radio bursts and their role in causing geomagnetic storms. In Section 2 we will describe the method of data analysis, Section 3 will present the results, and the conclusion will be drawn in Section 4.

2. Data Analysis

The data on DH-type-II bursts were obtained from Wind/WAVES type-II online catalog (http://cdaw.gsfc.nasa.gov/CME_list/radio/waves_type2.html) covering the period 1997–2008 and containing 344 events. The DH-type-II bursts are recorded in the frequency range between 14 MHz and 20 kHz using RAD-2 (14–1 MHz) and RAD-1 (1 MHz–20 kHz) instruments by the Radio and Plasma Wave (WAVES) experiment on board the Wind spacecraft [13]. The data regarding flares associated with DH-type-II bursts (start time, end time, and peak time) are provided by the GOES soft X-ray flare catalog (http://www.ngdc.noaa.gov/stp/space-weather/solar-data/solar-features/solar-flares/x-ray/goes). The data regarding the related CMEs (speed, width, and acceleration) are taken from the online SOHO/LASCO CME catalog [14] maintained by the CDAW data Center (http://cdaw.gsfc.nasa.gov/CME_list). Out of 344 events only 230 events are taken for our further analysis using the following selection criteria.(i)The given flare information should be clear (location and flare class should be reported).(ii)The data gaps and Backside events are excluded from the analysis.

The above two selection criteria are used to select the clear events from which the properties of CMEs and their associated DH-type-II bursts can be studied clearly. The DH-type-II bursts associated with flares and CMEs are listed in Wind/WAVES type-II online catalog; we make use of the catalog. The temporal time window between DH-type-II bursts with flares and CMEs is ±60 min form CME onset, but in some cases the time difference is longer; then the Type-II bursts start at very low frequency [15].

Recently Richardson and Cane [16] compiled a catalog of 340 ICMEs that passed Earth during 1996–2009. We utilized this ICME catalog for selecting the geoeffective events. We compared the CMEs listed in the ICME catalog [16] with 230 DH CMEs (DH-type-II bursts associated CMEs). The events are considered to be geoeffective if their Dst index ≤−50 nT [17]. A sample of 50 CMEs in the ICME catalog coincides with DH CMEs (their Dst index values are ≤−50 nT) and these 50 CMEs are termed geoeffective events. And the remaining 180 events are classified as nongeoeffective events.

Therefore the sample of 230 events (DH-type-II bursts associated with flares and CMEs) is compared with 340 ICMEs list [16]. The sample events are divided in to two groups as follows.(i)Geoeffective events: It contains 50 events, whose DH CMEs are listed in the ICME list [16] and corresponding Dst index values ≤−50 nT.(ii)Nongeoeffective events: It contains the remaining 180 events, whose DH CMEs are not listed in ICME list [16].

3. Results and Discussions

The properties of Type-II bursts and their associated flares and CMEs in the geoeffective and nongeoeffective events were summarized in Table 1. In Table 1, column 2 indicates the properties of Type-II bursts, flares, and CMEs, column 3 shows nongeoeffective, column 4 lists the geoeffective events, and column 5 represents the -test value, the statistical significance of mean values of geoeffective, and nongeoeffective events ( ≤ 5% means that there is 5% accidental difference is possible and the statistical significance is 95%).

Table 1: Properties of type-II bursts, flares, and CMEs in geoeffective and nongeoeffective events.

S. no.
Properties
Non-geoeffective events
Geoeffective events
-test value (%)

DH-type-II burst

1
Starting frequency (MHz)
10.14
10.99
21.32

2
Ending frequency (MHz)
2.38
1.52
7.09

3
Band width (MHz)
7.76
9.46
2.45

4
Duration (min)
288
958
0.007

Flares

5
Flare duration (min)
50
70
6.3

6
Flare rise time (min)
25.97
35.18
6.9

7
Flare decay time (min)
24.66
35.12
10.55

CMEs

8
CME speed (km s⁻¹)
1170
1263
35.39

9
Width (deg)
247
337
≪1

10
Acceleration (m s⁻²)
−4.25
−19.23
5.05

3.1. Properties of Type-II Bursts

The distributions of starting and ending frequency of geoeffective (right) and nongeoeffective events (left) associated with DH-type-II bursts are presented in Figures 1(a)–1(d). The type-II burst starting frequency indicates the height at which shocks are being formed from the eruption [18]. The starting frequency of DH-type-II bursts varies between 14 and 1 MHz, where 14 MHz is the upper cutoff frequency of the WAVES instrument. Figures 1(a) and 1(b) show the distribution of starting frequency of DH-type-II bursts associated with nongeoeffective events and geoeffective events. About 46% (82/180) of the nongeoeffective events and 54% (27/50) of the geoeffective events start at 14 MHz. The starting frequency of events at 14 MHz implies that they cover the whole range of the WAVES instrument and some of them may be a continuation of metric type-II bursts. The mean starting frequency of geoeffective events is 11 MHz and that of the nongeoeffective events is 10 MHz. The difference between the means is not statistically significant with -test value > 5% as seen in Table 1.

(a)

(b)

(c)

(d)

Figure 1: Distribution of starting frequency of DH-type-II bursts for (a) nongeoeffective eventsand (b) geoeffective events and distribution of ending frequency of DH-type-II bursts for (c) nongeoeffective events and (d) geoeffective events. In the Figure the geoeffective events are shown in right side and the nongeoeffective events on left side.

The type-II burst ending frequency indicates the energy of CMEs [18, 19]; that is, when the kinetic energy of the associated CMEs are more then the shock can travel to larger distance in the interplanetary medium. The distributions of ending frequency of nongeoeffective events (left) and geoeffective events (right) are presented in Figures 1(c) and 1(d), respectively. The end frequency varies between 12 MHz and 25 KHz. In nongeoeffective events 54% (87/180) ends below 1 MHz, while in geoeffective events 76% (38/50) ends below 1 MHz. Most of the geoeffective events end around/below 1 MHz implies that majority of the DH-type-II bursts continue to km wavelength range. The mean ending frequency of nongeoeffective events is 2 MHz and that of the geoeffective events is 1.5 MHz. In both cases the ending frequency is below 2 MHz which clearly indicates that the kinetic energy of the associated CMEs is larger, but they differ slightly in geoeffective and nongeoeffective events. The difference between the means is less statistically significant with -test value slightly greater than 5% as seen in Table 1. Therefore the geoeffective events have highest starting frequency and lowest ending frequency compared to nongeoeffective events associated with DH-type-II bursts.

Figures 2(a) and 2(b) show the distribution of durations (the difference between the starting and ending time of the DH-type-II burst) for nongeoeffective (left) and geoeffective events (right), respectively. The duration of the DH-type-II bursts varies between few min and 4000 min. In nongeoeffective events 76% (137/200) have duration within 200 min and the remaining 24% (43/180) have duration greater than 200 min; similarly for geoeffective events, 40% (20/50) have duration below 200 min and the remaining 60% (30/50) have duration greater than 200 min. The mean duration of the nongeoeffective events is 288 min and that of the geoeffective events is 958 min. The duration of the DH-type-II bursts is longer for geoeffective events than nongeoeffective events. The difference between the means is statistically significant with -test value < 1% as seen in Table 1.

(a)

(b)

(c)

(d)

Figure 2: Distribution of duration of DH-type-II bursts for (a) nongeoeffective events and (b) geoeffective events and bandwidth of DH-type-II bursts for (c) nongeoeffective events and (d) geoeffective events. In the Figure the geoeffective events are shown in right side and the nongeoeffective events on left side.

The distributions of bandwidths (the difference between starting and ending frequency of the DH-type-II burst) of nongeoeffective events (left) and geoeffective events (right) are shown in Figures 2(c) and 2(d), respectively. Majority of the DH-type-II bursts in both groups have bandwidths less than 13 MHz. Only 15% of nongeoeffective events (27/180) have bandwidth greater than 13 MHz. On other hand, 38% of geoeffective events (19/50) have bandwidth greater than 13 MHz. The mean bandwidth of nongeoeffective events is 8 MHz and that of the geoeffective events is 9 MHz. The difference between the means is statistically significant with -test value < 1% as seen in Table 1.

3.2. Properties of Associated Flares

The distributions of flare rise times (the difference between flare starting time and flare peaking time) for nongeoeffective events (left) and geoeffective events (right) are shown in Figures 3(a) and 3(b), respectively. The flare rise times can be used to establish the relation between flares-type-II bursts [20]. The flare rise times vary between few min and 180 min. In nongeoeffective events 72% of the flare peaks (129/180) within 30 min of the flare start, while in geoeffective events 66% (33/50) peaks within 30 min. The distribution decreases exponentially after the rise time in nongeoeffective events, while it is not a case for geoeffective events. The mean flare rise time of nongeoeffective events is 26 min and that of the geoeffective events is 35 min. Vršnak et al. [21] reported that the acceleration of CMEs showed a fundamental relationship between the dynamic of CMEs and flare energy release. The majority of the DH-type-II bursts are produced after the flare rise times; therefore they decelerate, while the DH-type-II bursts that occur before the flare rise times are found to accelerate. The difference between the means is less statistically significant with -test value slightly greater than 5% as seen in Table 1.

(a)

(b)

(c)

(d)

Figure 3: Distribution of flare rise time for (a) nongeoeffective events and (b) geoeffective events and flare decay time for (c) nongeoeffective events and (d) geoeffective events. In the Figure the geoeffective events are shown in right side and the nongeoeffective events on left side.

Figures 3(c) and 3(d) show the distribution of flare decay times (the difference between flare peaking and flare ending time) for nongeoeffective events (left) and geoeffective events (right), respectively. The decay times of the flare varies between few min and 180 min. In nongeoeffective events 75% (135/180) of the flares decay within 30 min, while in geoeffective events 62% (31/50) of the flares decay within 30 min. The mean decay times of nongeoeffective events is 25 min and that of the geoeffective events is 35 min. The difference between the means is less statistically significant with t-test value slightly greater than 5% as seen in Table 1.

The distributions of flare durations (the difference between flare starting time and flare ending time) for nongeoeffective (left) and geoeffective events (right) are shown in Figures 4(a) and 4(b), respectively. In nongeoeffective events 61% (110/180) have duration within 50 min, while in geoeffective events 54% (27/50) have duration within 50 min. The mean flare duration of non-geoeffective events is 50 min and that of the geoeffective events is 70 min. The flare duration of geoeffective events is found to be longer than that of nongeoeffective events. The longer flare duration or rise time is an implication of enhanced action of Lorentz force which indicates that the associated CME may have high speed and acceleration [22]. The difference between the means is less statistically significant with -test value slightly greater than 5% as seen in Table 1.

(a)

(b)

(c)

(d)

Figure 4: Distribution of flare duration for (a) nongeoeffective events and (b) geoeffective events and flare class for (c) nongeoeffective events and (d) geoeffective events. In the Figure the geoeffective events are shown in right side and the nongeoeffective events on left side.

The distributions of flare classes associated with CMEs producing DH-type-II bursts for nongeoeffective (left) and geoeffective events (right) are shown in Figures 4(c) and 4(d), respectively. The X-ray flare class is classified as , , , , and depending on their intensities: where (, , , , ), the value after the flare class is the multiplication factor. For example, 5.4 flare has a intensity value of . In nongeoeffective events 23% (41/180) are -Class flares, 53% (96/180) are -Class flares, 21% (37/180) are -Class flares, and 3% (6/180) are -Class flares, while in geoeffective events 40% (20/50) are -Class flares, 38% (19/50) are -Class flares, and the remaining 22% (11/50) are -Class flares. The geoeffective events are associated with more energetic -Class flares than nongeoeffective events. The association rate of flare class increases with flux of the flares [23, 24]. The CMEs associated with stronger flares will have high CME speed [25–27]. About 68% of the geoeffective events (36/50) and 60% of the nongeoeffective events (108/180) originate on the western hemisphere. The western source regions are better candidate for CMEs to be geoeffective [28].

3.3. Properties of Associated CMEs

The distributions of CME speed for nongeoeffective (left) and geoeffective events (right) are shown in Figures 5(a) and 5(b), respectively. The CME speed listed in the LASCO CME catalog is measured from the height time measurements projected in the sky plane. So all the measured parameters will suffer from projection effects; no attempt had been made to correct the projection effects. The speed of the CMEs varies from few hundred km s⁻¹ to 3000 km s⁻¹. The mean speed of nongeoeffective events is 1170 km s⁻¹ and that of the geoeffective events is 1263 km s⁻¹. The difference between the means is not statistically significant with -test value > 5% as seen in Table 1.

(a)

(b)

(c)

(d)

(e)

(f)

Figure 5: Distribution of speed of CMEs for (a) nongeoeffective events and (b) geoeffective events, width of CMEs for (c) nongeoeffective events and (d) geoeffective events, and acceleration of CMEs for (e) nongeoeffective events and (f) geoeffective events. In the Figure the geoeffective events are shown in right side and the nongeoeffective events on left side.

The distributions of apparent width of nongeoeffective (left) and geoeffective events (right) are presented in Figures 5(c) and 5(d), respectively. The angular width is the angular extent between the two edge position angles of the CME in the sky plane. The width of the CMEs varies between 30° and 360°. The mean width of the nongeoeffective events is 247° and that of the geoeffective events is 337°. The difference between the means is statistically significant with -test value < 1% as seen in Table 1. In geoeffective events 88% (44/50) are halo CMEs, while in nongeoeffective events only 46% (83/180) are halo CMEs. Therefore the geoeffective events are found to be wider than nongeoeffective events.

The distributions of CME acceleration for nongeoeffective (left) and geoeffective events (right) are presented in Figures 5(e) and 5(f), respectively. We considered the CMEs with data point ≥4, so that the acceleration is reliable. From the distributions it is clear that in both the geoeffective and nongeoeffective events tend to extend on decelerating side shows the tendency of CMEs to decelerate, while few nongeoeffective events show acceleration. The CMEs will accelerate/decelerate in the LASCO FOV depending on the CMEs interaction with the solar wind. The fast CMEs tend to decelerate, while the slow CMEs accelerate [14]. The mean acceleration of nongeoeffective events is −4.25 m s⁻² and that of the geoeffective events is −19.23 m s⁻². The difference between the means is less statistically significant with -test value slightly greater than 5% as seen in Table 1.

The correlations between CME speed and CME acceleration for nongeoeffective (left) and geoeffective events (right) associated with DH-type-II bursts are shown in Figures 6(a) and 6(b), respectively. There exists a good correlation between CME speed and acceleration for geoeffective events with correlation coefficient of , while no clear correlation exists for nongeoeffective events. Our result is similar to Gopalswamy et al. [11], who reported the properties of CMEs in limb and all events associated with DH-type-II bursts. Majority of the CMEs considered by Gopalswamy et al. [11] are decelerating events; therefore the acceleration is anticorrelated with the CME speed, which shows that the fast CMEs decelerate more. From Figure 6(b), it is clear that the acceleration decreases with increase in speed of CMEs; that is, the faster CMEs decelerate more than slower CMEs. Gopalswamy et al. [18] concluded that the faster CMEs decelerate more because of the drag force faced by the CMEs as they propagate in the interplanetary medium. The stronger flare associated CMEs are highly decelerated in LASCO FOV [26]. The relationship between CME speed and CME acceleration were studied by several authors [11, 14, 21, 29] in which acceleration increases with speed, while in our result the CME decelerates (acceleration decreases) with increase in CME speed and the anticorrelation is due to the aerodynamical drag [24, 30–33]. The action of Lorentz force plays an important role in acceleration/deceleration of CMEs. Longer action of Lorentz force is found in accelerating CMEs, while it acts shorter in decelerating CMEs. As a result the drag force dominates the dynamic of CMEs with decrease in Lorentz and gravity force, and the CMEs decelerate in the LASCO FOV [21]. The anticorrelation between CME speed and acceleration is consistent with the earlier reports [14, 21, 33]. Yashiro et al. [14] reported that CME speed (>900 km/s) tends to decelerate in the LASCO FOV.

(a)

(b)

Figure 6: Correlation between CMEs speed and acceleration of CMEs for (a) nongeoeffective events and (b) geoeffective events. In the Figure the geoeffective events are shown in right side and the nongeoeffective events on left side.

The arrival time of CMEs at earth can be predicted using empirical models [34, 35]. The CME speed changes in interaction with the solar wind speed. The arrival time model uses the CME speed as the primary input and estimates the travel time of CMEs at earth. The fast CMEs decelerating in the LASCO FOV will arrive with shorter travel time than slow CMEs, which have longer travel time. The arrival time predicted by model also contains error, since the CMEs observed and listed by LASCO CME catalog suffer from projection effects. If the projection effects are corrected then the error in estimating the arrival time also decreases.

The correlations between CME speed and flare flux for nongeoeffective (left) and geoeffective events (right) are shown in Figures 7(a) and 7(b), respectively. The value of flare flux is obtained from the X-ray flare class; the value after the flare class is the multiplication factor. For example, 5.4 has a flux of . The correlation is used to investigate the flare-CME relationship. The relation between strength of the flare and CME speed was studied by several authors [36–40]. We found a similar relation between the two parameters. There exists a weak correlation between CME speed and flare flux for nongeoeffective events () and good correlation for geoeffective events (). The correlation shows that the faster CMEs are associated with more energetic flares. Earlier report by Moon et al. [26] found a correlation coefficient of between flare flux and CME speed, while Yashiro and Gopalswamy [41] reported a better correlation coefficient of . The stronger flares are associated with faster CMEs in the geoeffective events, while the weak correlation in the nongeoeffective events is due to the lack of stronger flares.

(a)

(b)

Figure 7: Correlation between CMEs speed and flare flux for (a) nongeoeffective events and (b) geoeffective events. In the Figure the geoeffective events are shown in right side and the nongeoeffective events on left side.

The correlations between CME acceleration and flare flux for nongeoeffective (left) and geoeffective events (right) are shown in Figures 8(a) and 8(b), respectively. There exists a good correlation between flare flux and CME acceleration for geoeffective events with a correlation coefficient of , while no clear correlation exists for nongeoeffective events. The CMEs associated with stronger flares are highly decelerated due to dominant action of drag force. Maričić et al. [39] obtained a good positive correlation between CME peak acceleration and flare flux during the acceleration phase.

(a)

(b)

Figure 8: Correlation between CMEs acceleration and flare flux for (a) nongeoeffective events and (b) geoeffective events. In the Figure the geoeffective events are shown in right side and the nongeoeffective events on left side.

The disturbance in the earth magnetic field caused by the impact of interplanetary magnetic field with enhanced southward magnetic field component is termed as Geomagnetic storms. The average change in horizontal component of earth’s magnetic field measured in nT at low latitude is known as disturbance storm time (Dst). The minimum Dst index value is the intensity of the storm. The geomagnetic storms are classified as weak (−30 nT ≤ Dst ≤ −50 nT), moderate (−50 nT ≤ Dst ≤ −100 nT), intense (−100 nT ≤ Dst < −200 nT), severe (−200 nT ≤ Dst ≤ −350 nT), and super storm (Dst < −350 nT) [42]. The CMEs with Dst ≤ −50 nT are considered to be geoeffective [17]. The distribution of Dst index and correlation between CME speed and Dst index for geoeffective events are presented in Figures 9(a) and 9(b), respectively. In Figure 9(a) the Dst value varies between −50 nT and −400 nT with mean Dst index (−150 nT). Therefore the mean value is found to be intense geoeffective.

(a)

(b)

Figure 9: (a) Distribution of Dst index for geoeffective events and (b) correlation between CMEs speed and Dst index for geoeffective events.

There exists a weak correlation between CME speed and Dst index with a correlation coefficient of as shown in Figure 9(b); the anticorrelation indicates that the Dst value decreases with increase in CME speed. Our result is similar to that of Gopalswamy et al. [43]. They investigated the dependence of geoeffectiveness with CME speed and they obtained a weak correlation with correlation coefficient of . The weak correlation indicates that the geoeffectiveness weakly depends on CME speed.

There exists a good correlation between Dst index and southward magnetic field component () with a correlation coefficient of as shown in Figure 10(a). The very less scattering in the correlation plot shows that there exists a relationship between Dst index and ; the geoeffectiveness strongly depends on values. The intense corresponds to intense geomagnetic storm. Therefore the south magnetic field component plays an important role in the generation of geomagnetic storms.

(a)

(b)

Figure 10: Correlation between (a) Dst index and southward magnetic field component () and (b) Dst index and solar wind speed for geoeffective events.

The correlation between solar wind speed and Dst index for geoeffective events are shown in Figure 10(b); there exists a good anticorrelation between Dst index and solar wind speed with correlation coefficient of , excluding the two outliers. The less scattering in the correlation plot shows that there exists a relationship between them and the geoeffectiveness depends on solar wind speed in the interplanetary medium. The fast solar winds are found to be associated with intense geomagnetic storm.

The correlation between CME speed and solar wind speed for geoeffective events are shown in Figure 11(a). There exists a good correlation with a correlation coefficient of , excluding the two outlier points. The correlation shows that there is a relationship between the CME speed and solar wind speed. Therefore the CME speed in the interplanetary medium is affected by the solar wind speed. The fast CMEs are found to have more solar wind speed.

(a)

(b)

Figure 11: Correlation between (a) CME speed and solar wind speed and (b) CME speed and southward magnetic field component () for geoeffective events.

The correlation between CME speed and are shown in Figure 11(b). No correlation exists between them.

Therefore it is concluded that the geoeffectiveness of the CMEs strongly depend on interplanetary parameters such as solar wind speed and and weakly depend on CME speed. The main cause for the arrival of geomagnetic storms at earth is intense and long duration and solar wind speed.

4. Conclusion

We have analyzed 230 CMEs associated with flares and DH-type-II bursts observed during 1997–2008. The sample events are divided into two groups based on the CMEs association with geomagnetic storm Dst ≤ −50 nT listed in the ICME catalog [16] as (i) geoeffective events and (ii) nongeoeffective events. The results of our study are summarized as follows.(i)The DH-type-II bursts associated with geoeffective events are found to have high starting frequency, low ending frequency, and long duration compared to the DH-type-II bursts associated with nongeoeffective events.(ii)The geoeffective events are associated with more energetic -Class flares than nongeoeffective events.(iii)The geoeffective events are found to have faster and wider CMEs than the nongeoeffective events.(iv)There exists a good correlation between CME speed and acceleration for geoeffective events with correlation coefficient of , while no clear correlation exists for nongeoeffective events.(v)There exists a good correlation between flare flux and CME acceleration for geoeffective events with a correlation coefficient of , while no clear correlation exists for nongeoeffective events.(vi)The correlation between CME speed and flare flux is good for geoeffective events () and weak for nongeoeffective events ().(vii)The geoeffective events are found to be associated with intense geomagnetic storm with mean Dst index (−150 nT).(viii)There exists a weak correlation between CME speed and Dst with a correlation coefficient of .(ix)There exists a good correlation between (i) Dst index and solar wind speed with a correlation coefficient of , (ii) Dst index and southward magnetic field component with a correlation coefficient of , and (iii) CME speed and solar wind speed with a correlation coefficient of .It is concluded that the intense and long duration southward magnetic field component () and fast solar wind speed are responsible for geomagnetic storms; the geomagnetic storms weakly depend on CME speed since they are altered by solar wind in the interplanetary medium. The faster and wider CMEs are more energetic and drive shocks in the outer corona [11]. About 22% of the DH-type-II bursts are associated with geomagnetic storms. Therefore the energetic CMEs that in turn produce the DH-type-II bursts are found to be associated with major flares. These DH-type-II bursts associated CMEs are good indicator of geomagnetic storms.

Acknowledgment

The authors greatly acknowledge the various online data centers of NOAA and NASA. They thank the Wind/WAVES team for providing the Type II catalog. The CME catalog used is provided by the center for solar physics and space weather and the catholic university of America in cooperation with Naval Research Laboratory and NASA. V. Vasanth thanks UGC-BSR for a meritorious fellowship.

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