發布時間: 2013 May 17 1307 UTC
Major flares expected (X-class flares expected, probability >=50%)
Active conditions expected (A>=20 or K=4)
Proton event in progress (>10 MeV)
| 10公分通量 | Ap | |
|---|---|---|
| 17 May 2013 | 149 | 014 |
| 18 May 2013 | 150 | 007 |
| 19 May 2013 | 152 | 013 |
Two M-class flares in past 24h, both from NOAA AR 1748. The first one occurred on May 16 at 21:53 UT, with intensity M1.3. The second flare was an M3.2 and peaked at 08:57 UT on May 17. This AR has still potential for producing X class flares. It maintains its beta-gamma-delta magnetic configuration, even though some fragmentation is seen in the trailing region and there are some indications that polarities are separating within the delta spot penumbra. The M3.2 flare of today was related to radio bursts and a CME. SWAP detected clear dimmings and an EIT wave around NOAA AR1748. There are no LACO data available yet, but a CME is indeed seen in STEREO COR2 data, it can be Earth directed. The speed in COR2-B is calculated to be 1300 km/s, making a possible arrival to the Earth on May 19 around noon. Protons levels (10MeV) are still above threshold, stable around 3 protons/cm2-s-sr. Geomagnetic conditions have been unsettled to active, due to long lasting periods of slow solar wind with sustained mild negative Bz (around -5nT). These are not related to the arrival of the CME of May 15, which is still not visible in ACE data, and may still arrive later today and produce storm levels (estimated max K = 6). As a reminder, this series of CMEs related to AR 1748 had a source region within 30 degrees of the solar limb, which reduces their possibility of arrival to the Earth to around 30%.
今日估計的國際太陽黑子數(ISN):124,基於10個觀測站。
| 卡塔尼亞沃爾夫數 | /// |
| 10厘米太陽通量 | 145 |
| AK Chambon La Forêt | 028 |
| AK Wingst | 024 |
| 估計地磁Ap指數 | 023 |
| 估計國際太陽黑子數 | 142 - 基於16個觀測站 |
| 日 | 開始 | 最大值 | 結束 | 位置 | 強度 | OP | 10cm | 卡塔尼亞天體物理觀測站/美國國家海洋暨大氣管理局 | 電波爆發類型 |
|---|---|---|---|---|---|---|---|---|---|
| 17 | 0843 | 0857 | 0919 | N12E57 | M3.2 | 2B | 450 | 75/1748 | IV/2II/2 |
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