ðɪs dɪstʃˈɑːɹdʒ ɪz ɹˈʌfli ɪkwˈɪvələnt tə fˈɪfti pɚsˈɛnt ʌvðə ɡlˈoʊbəl dɪstʃˈɑːɹdʒ dˈʊɹɹɪŋ mˈɛltwɔːɾɚ pˈʌls wˈʌn ˈeɪ. ðɪs ɹᵻsˈɜːtʃ ˈɔːlsoʊ ʃˈoʊz ðætðə mˌɪsɪsˈɪpi mˈɛltwɔːɾɚ flˈʌd ˌɛmdˌʌbəljˌuːˈɛf fˈoːɹ əkˈɜːd dˈʊɹɹɪŋ ðɪ ˈælɚɹˌɑːd ˌɑːsɪlˈeɪʃən ænd hæd lˈɑːɹdʒli stˈɑːpt bᵻfˌoːɹ ðə bɪɡˈɪnɪŋ ʌvðə jˈʌŋɡɚ dɹˈaɪəz stˈeɪdɪəl.
This discharge is roughly equivalent to 50% of the global discharge during meltwater pulse 1A. This research also shows that the Mississippi meltwater flood MWF-4 occurred during the Allerød oscillation and had largely stopped before the beginning of the Younger Dryas stadial.